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true, "dateFieldsTimeReference": null, "preferredTimeReference": null, "datesInUnknownTimezone": false, "hasMetadata": true, "isDataArchived": false, "archivingInfo": { "supportsQueryWithHistoricMoment": false, "startArchivingMoment": -1 }, "supportsCoordinatesQuantization": true, "supportsDynamicLegends": false }, { "currentVersion": 11.3, "cimVersion": "3.3.0", "id": 16, "name": "Signaalkaart overstroming", "type": "Raster Layer", "description": "

De Signaalkaart Klimaatadaptatie bebouwing overstroming is gebaseerd op verschillende onderliggende signaalkaarten voor de geschiktheid van (toekomstige) ruimtelijke ontwikkelingen. Deze kaart signaleert welke gebieden meer of minder geschikt zijn voor een beoogde functie. In de signaalkaarten is de relatie gelegd tussen het huidige bodem en watersysteem, klimaatverandering en (toekomstig) landgebruik. In deze kaart is de geschiktheid voor woningbouw vanuit overstromingsrisico\u2019s in beeld gebracht. We kijken daarbij naar plaatselijke overstromingskans en optredende waterdiepte. Zo worden slachtoffers zoveel mogelijk worden voorkomen en schade aan infrastructuur beperkt Langs dijken en duinen is ruimte nodig voor toekomstige versterking. <\/SPAN><\/SPAN><\/P>

De kaart is tot stand gekomen op basis van expert judgement en afstemming vanuit PNH / HHNK / AGV. De signaalkaart is gebaseerd op de volgende brondata: <\/SPAN><\/P>

Plaatsgebonden overstromingskans norm 2050 (LIWO, 2022), Inundatie buitendijkse gebieden kleine kans (LIWO, 2022), Primaire keringen (LIWO, 2022), Regionale keringen, (LIWO 2022), Beschermingszone (PDOK, 2022),Oeverlanden van Amsterdam-Rijnkanaal en Noordzeekanaal (Defacto Stedenbouw, 2022) <\/SPAN><\/SPAN><\/P><\/TD><\/TR>

Bewerking: RHDHV, Defacto 2023<\/SPAN><\/P><\/TD><\/TR>

Inhoudelijk eigenaar PNH: Annebet van Duinen, BEL/OMB<\/SPAN><\/P><\/TD><\/TR>

<\/TD><\/TR><\/TBODY><\/TABLE>

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Deze kaart toont de verwachte overstromingskans in 2050 waarbij een waterdiepte van meer dan 20 cm optreedt, veroorzaakt door een doorbraak van een waterkering langs het hoofd- of het regionale watersysteem of bij overstromen van onbeschermde gebieden. Deze kaart geeft dus de totale kans op alle mogelijk overstromingen weer ongeacht de resulterende overstromingsdiepte. Alle primaire waterkeringen voldoen daarbij exact aan de overstromingskansnorm in de Waterwet. Voor regionale waterkeringen is de provinciale overschrijdingskans norm als overstromingskans gehanteerd. De faalkans van primaire waterkeringen zijn onafhankelijk verondersteld. De faalkans van primaire waterkeringen zijn ingeschat op basis van de vigerende faaldefinitie en zonder noodmaatregelen.<\/SPAN><\/SPAN><\/P>

Label B - Gebieden met een overstromingsdiepte van 20 - 50 cm - Voorkom schade in gebieden met een overstromingsdiepte van 20 tot 50 cm. Dit vraagt om aanvullende randvoorwaarden voor ontwikkelingen, zoals aangepast bouwen en hogere aansluitingen elektra, die naar verwachting goed uitvoerbaar zijn. Elke locatie vraagt uiteindelijk om een meer gedetailleerde benadering die kan leiden tot een combinatie van handelingsperspectieven. (value >1, <=3)<\/SPAN><\/P><\/DIV><\/DIV><\/DIV>", "geometryType": null, "copyrightText": "", "parentLayer": { "id": 3, "name": "Overstroming" }, "subLayers": [], "minScale": 0, "maxScale": 0, "defaultVisibility": false, "extent": { "xmin": 94110, "ymin": 464251.91299999994, "xmax": 150060, "ymax": 577776.913, "spatialReference": { "wkid": 28992, "latestWkid": 28992, "xyTolerance": 0.001, "zTolerance": 0.001, "mTolerance": 0.001, "falseX": -30515500, "falseY": -30279500, "xyUnits": 10000, "falseZ": -100000, "zUnits": 10000, "falseM": -100000, "mUnits": 10000 } }, "hasAttachments": false, "htmlPopupType": "esriServerHTMLPopupTypeNone", "displayField": "", "typeIdField": null, "subtypeFieldName": null, "subtypeField": null, "defaultSubtypeCode": null, "fields": null, "geometryField": {}, "indexes": [], "subtypes": [], "relationships": [], "canModifyLayer": false, "canScaleSymbols": false, "hasLabels": false, "capabilities": "Map,Query", "supportsStatistics": false, "supportsExceedsLimitStatistics": false, "supportsAdvancedQueries": false, "supportedQueryFormats": "JSON, geoJSON, PBF", "isDataVersioned": false, "ownershipBasedAccessControlForFeatures": {"allowOthersToQuery": true}, "useStandardizedQueries": true, "advancedQueryCapabilities": { "useStandardizedQueries": true, "supportsStatistics": false, "supportsPercentileStatistics": false, "supportsHavingClause": false, "supportsOrderBy": false, "supportsDistinct": false, "supportsCountDistinct": false, "supportsAdvancedQueryRelated": true, "supportsQueryRelatedPagination": true, "supportsPagination": false, "supportsLod": false, "supportsQueryWithLodSR": false, "supportsTrueCurve": true, "supportsQueryWithDatumTransformation": true, "supportsReturningQueryExtent": true, "supportsQueryWithDistance": true, "supportsSqlExpression": false, "supportsTimeRelation": true, "supportsSqlFormat": false, "supportsQueryAnalytic": false, "supportsCurrentUserQueries": true }, "supportsDatumTransformation": true, "dateFieldsTimeReference": null, "preferredTimeReference": null, "datesInUnknownTimezone": false, "hasMetadata": true, "isDataArchived": false, "archivingInfo": { "supportsQueryWithHistoricMoment": false, "startArchivingMoment": -1 }, "supportsCoordinatesQuantization": true, "supportsDynamicLegends": true }, { "currentVersion": 11.3, "cimVersion": "3.3.0", "id": 13, "name": "Label C: Gebieden langs het ARK-NZK kanaal gebied", "type": "Feature Layer", "description": "

Deze kaart toont oeverlanden van het Amsterdam-Rijnkanaal en Noordzeekanaal. <\/SPAN><\/P>

Label C - Houd rekening met toenemende waterstanden hoofdwatersysteem (ontwikkel aangepast). De waterstanden van het hoofdwatersysteem (Amsterdam-Rijnkanaal, Noordzeekanaal, het Markermeer en IJsselmeer) zullen in de toekomst mogelijk worden verhoogd om voldoende water te kunnen bergen ( voor de waterafvoer of zoetwaterbeschikbaarheid). 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Deze kaart toont de verwachte overstromingskans in 2050 waarbij een waterdiepte van meer dan 200 cm optreedt, veroorzaakt door een doorbraak van een waterkering langs het hoofd- of het regionale watersysteem of bij overstromen van onbeschermde gebieden. Deze kaart geeft dus de totale kans op alle mogelijk overstromingen weer ongeacht de resulterende overstromingsdiepte. Alle primaire waterkeringen voldoen daarbij exact aan de overstromingskansnorm in de Waterwet. Voor regionale waterkeringen is de provinciale overschrijdingskans norm als overstromingskans gehanteerd. De faalkans van primaire waterkeringen zijn onafhankelijk verondersteld. De faalkans van primaire waterkeringen zijn ingeschat op basis van de vigerende faaldefinitie en zonder noodmaatregelen.<\/SPAN><\/SPAN><\/P>

Label D - Overstromingsdiepte van meer dan 200 cm en een kans > 1/1000 jaar - Heroverweeg locatiekeuze van ontwikkelingen in binnendijkse gebieden met diepe overstroming (> 200 cm) en kans groter dan 1:1.000. Ontwikkelingen in deze gebieden leggen (ook met adaptatiemogelijkheden) mogelijk een claim op de toekomst en vragen om een heroverweging van de locatiekeuze. Elke locatie vraagt uiteindelijk om een meer gedetailleerde benadering die kan leiden tot een combinatie van handelingsperspectieven.<\/SPAN><\/SPAN><\/P>

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Deze kaart toont de verwachte overstromingskans in 2050 waarbij een waterdiepte van meer dan 50 cm optreedt, veroorzaakt door een doorbraak van een waterkering langs het hoofd- of het regionale watersysteem of bij overstromen van onbeschermde gebieden. Deze kaart geeft dus de totale kans op alle mogelijk overstromingen weer ongeacht de resulterende overstromingsdiepte. Alle primaire waterkeringen voldoen daarbij exact aan de overstromingskansnorm in de Waterwet. Voor regionale waterkeringen is de provinciale overschrijdingskans norm als overstromingskans gehanteerd. De faalkans van primaire waterkeringen zijn onafhankelijk verondersteld. De faalkans van primaire waterkeringen zijn ingeschat op basis van de vigerende faaldefinitie en zonder noodmaatregelen.<\/SPAN><\/SPAN><\/P>

Label C - Overstromingsdiepte van 50 tot 200 cm en een kans < 1/1000 jaar - Zet in op schuilen en evacueren in gebieden met overstroming (> 50 cm) en kans kleiner dan 1:1.000. In deze gebieden moet extra aandacht uitgaan naar gevolgbeperking voor vitale en kwetsbare functies. Elke locatie vraagt uiteindelijk om een meer gedetailleerde benadering die kan leiden tot een combinatie van handelingsperspectieven.<\/SPAN><\/SPAN><\/P>

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Deze kaart toont de verwachte overstromingskans in 2050 waarbij een waterdiepte van meer dan 200 cm optreedt, veroorzaakt door een doorbraak van een waterkering langs het hoofd- of het regionale watersysteem of bij overstromen van onbeschermde gebieden. Deze kaart geeft dus de totale kans op alle mogelijk overstromingen weer ongeacht de resulterende overstromingsdiepte. Alle primaire waterkeringen voldoen daarbij exact aan de overstromingskansnorm in de Waterwet. Voor regionale waterkeringen is de provinciale overschrijdingskans norm als overstromingskans gehanteerd. De faalkans van primaire waterkeringen zijn onafhankelijk verondersteld. De faalkans van primaire waterkeringen zijn ingeschat op basis van de vigerende faaldefinitie en zonder noodmaatregelen.<\/SPAN><\/SPAN><\/P>

Label D - Overstromingsdiepte van meer dan 200 cm en een kans > 1/1000 jaar - Heroverweeg locatiekeuze van ontwikkelingen in binnendijkse gebieden met diepe overstroming (> 200 cm) en kans groter dan 1:1.000. Ontwikkelingen in deze gebieden leggen (ook met adaptatiemogelijkheden) mogelijk een claim op de toekomst en vragen om een heroverweging van de locatiekeuze. Elke locatie vraagt uiteindelijk om een meer gedetailleerde benadering die kan leiden tot een combinatie van handelingsperspectieven.<\/SPAN><\/SPAN><\/P>

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Deze kaart toont de verwachte overstromingskans in 2050 waarbij een waterdiepte van meer dan 200 cm optreedt, veroorzaakt door een doorbraak van een waterkering langs het hoofd- of het regionale watersysteem of bij overstromen van onbeschermde gebieden. Deze kaart geeft dus de totale kans op alle mogelijk overstromingen weer ongeacht de resulterende overstromingsdiepte. Alle primaire waterkeringen voldoen daarbij exact aan de overstromingskansnorm in de Waterwet. Voor regionale waterkeringen is de provinciale overschrijdingskans norm als overstromingskans gehanteerd. De faalkans van primaire waterkeringen zijn onafhankelijk verondersteld. De faalkans van primaire waterkeringen zijn ingeschat op basis van de vigerende faaldefinitie en zonder noodmaatregelen.<\/SPAN><\/SPAN><\/P>

Label D - Overstromingsdiepte van meer dan 200 cm en een kans < 1/1000 jaar - Zet in op schuilen en evacueren in binnendijkse gebieden met diepe overstroming (> 200 cm) en kans kleiner dan 1:1.000. Bebouwing in deze gebieden legt (ook met adaptatiemogelijkheden) mogelijk een claim op de toekomst. Dit vraagt om maatregelen voor gevolgbeperking: inzetten op schuilen en evacueren en extra aandacht voor vitale en kwetsbare functies. Elke locatie vraagt uiteindelijk om een meer gedetailleerde benadering die kan leiden tot een combinatie van handelingsperspectieven.<\/SPAN><\/P><\/DIV><\/DIV><\/DIV>", "geometryType": null, "copyrightText": "", "parentLayer": { "id": 3, "name": "Overstroming" }, "subLayers": [], "minScale": 0, "maxScale": 0, "defaultVisibility": false, "extent": { "xmin": 94110, "ymin": 464251.91299999994, "xmax": 150060, "ymax": 577776.913, "spatialReference": { "wkid": 28992, "latestWkid": 28992, "xyTolerance": 0.001, "zTolerance": 0.001, "mTolerance": 0.001, "falseX": -30515500, "falseY": -30279500, "xyUnits": 10000, "falseZ": -100000, "zUnits": 10000, "falseM": -100000, "mUnits": 10000 } }, "hasAttachments": false, "htmlPopupType": "esriServerHTMLPopupTypeNone", "displayField": "", "typeIdField": null, "subtypeFieldName": null, "subtypeField": null, "defaultSubtypeCode": null, "fields": null, "geometryField": {}, "indexes": [], "subtypes": [], "relationships": [], "canModifyLayer": false, "canScaleSymbols": false, "hasLabels": false, "capabilities": "Map,Query", "supportsStatistics": false, "supportsExceedsLimitStatistics": false, "supportsAdvancedQueries": false, "supportedQueryFormats": "JSON, geoJSON, PBF", "isDataVersioned": false, "ownershipBasedAccessControlForFeatures": {"allowOthersToQuery": true}, "useStandardizedQueries": true, "advancedQueryCapabilities": { "useStandardizedQueries": true, "supportsStatistics": false, "supportsPercentileStatistics": false, "supportsHavingClause": false, "supportsOrderBy": false, "supportsDistinct": false, "supportsCountDistinct": false, "supportsAdvancedQueryRelated": true, "supportsQueryRelatedPagination": true, "supportsPagination": false, "supportsLod": false, "supportsQueryWithLodSR": false, "supportsTrueCurve": true, "supportsQueryWithDatumTransformation": true, "supportsReturningQueryExtent": true, "supportsQueryWithDistance": true, "supportsSqlExpression": false, "supportsTimeRelation": true, "supportsSqlFormat": false, "supportsQueryAnalytic": false, "supportsCurrentUserQueries": true }, "supportsDatumTransformation": true, "dateFieldsTimeReference": null, "preferredTimeReference": null, "datesInUnknownTimezone": false, "hasMetadata": true, "isDataArchived": false, "archivingInfo": { "supportsQueryWithHistoricMoment": false, "startArchivingMoment": -1 }, "supportsCoordinatesQuantization": true, "supportsDynamicLegends": true }, { "currentVersion": 11.3, "cimVersion": "3.3.0", "id": 8, "name": "Label E: Inundatie buitendijkse gebieden", "type": "Raster Layer", "description": "

Deze kaart toont gebieden met \"Label E - Inundatie buitendijkse keringen\" van de Signaalkaart bebouwing - overstroming met als beschrijving:<\/SPAN><\/P>

\"Heroverweeg buitendijkse ontwikkelingen langs het IJsselmeer en Markermeer. Ruimtelijke ontwikkelingen in buitendijkse gebieden langs de kust, het IJsselmeer en het Markermeer die de huidige of toekomstige bergingscapaciteit van de meren beperken zijn niet wenselijk.\"<\/SPAN><\/P>

Deze waterdieptekaart toont welke onbeschermde gebieden langs het primaire watersysteem tot ongeveer eens in de tienduizend jaar kunnen overstromen. De kaart geeft mogelijke overstromingen weer die in werkelijkheid niet allemaal tegelijkertijd zullen optreden. <\/SPAN><\/P><\/DIV><\/DIV><\/DIV>", "geometryType": null, "copyrightText": "", "parentLayer": { "id": 3, "name": "Overstroming" }, "subLayers": [], "minScale": 0, "maxScale": 0, "defaultVisibility": false, "extent": { "xmin": 94100, "ymin": 464250, "xmax": 150075, "ymax": 577775, "spatialReference": { "wkid": 28992, "latestWkid": 28992, "xyTolerance": 0.001, "zTolerance": 0.001, "mTolerance": 0.001, "falseX": -30515500, "falseY": -30279500, "xyUnits": 10000, "falseZ": -100000, "zUnits": 10000, "falseM": -100000, "mUnits": 10000 } }, "hasAttachments": false, "htmlPopupType": "esriServerHTMLPopupTypeNone", "displayField": "Value", "typeIdField": null, "subtypeFieldName": null, "subtypeField": null, "defaultSubtypeCode": null, "fields": [ { "name": "objectid", "type": "esriFieldTypeOID", "alias": "objectid", "domain": null }, { "name": "value", "type": "esriFieldTypeInteger", "alias": "value", "domain": null }, { "name": "count", "type": "esriFieldTypeDouble", "alias": "count", "domain": null } ], "geometryField": {}, "indexes": [ { "name": "r3999_sde_rowid_uk", "fields": "objectid", "isAscending": true, "isUnique": true, "description": "" } ], "subtypes": [], "relationships": [], "canModifyLayer": false, "canScaleSymbols": false, "hasLabels": false, "capabilities": "Map,Query", "supportsStatistics": false, "supportsExceedsLimitStatistics": false, "supportsAdvancedQueries": false, "supportedQueryFormats": "JSON, geoJSON, PBF", "isDataVersioned": false, "ownershipBasedAccessControlForFeatures": {"allowOthersToQuery": true}, "useStandardizedQueries": true, "advancedQueryCapabilities": { "useStandardizedQueries": true, "supportsStatistics": false, "supportsPercentileStatistics": false, "supportsHavingClause": false, "supportsOrderBy": false, "supportsDistinct": false, "supportsCountDistinct": false, "supportsAdvancedQueryRelated": true, "supportsQueryRelatedPagination": true, "supportsPagination": false, "supportsLod": false, "supportsQueryWithLodSR": false, "supportsTrueCurve": true, "supportsQueryWithDatumTransformation": true, "supportsReturningQueryExtent": true, "supportsQueryWithDistance": true, "supportsSqlExpression": false, "supportsTimeRelation": true, "supportsSqlFormat": false, "supportsQueryAnalytic": false, "supportsCurrentUserQueries": true }, "supportsDatumTransformation": true, "dateFieldsTimeReference": null, "preferredTimeReference": null, "datesInUnknownTimezone": false, "hasMetadata": true, "isDataArchived": false, "archivingInfo": { "supportsQueryWithHistoricMoment": false, "startArchivingMoment": -1 }, "supportsCoordinatesQuantization": true, "supportsDynamicLegends": true }, { "currentVersion": 11.3, "cimVersion": "3.3.0", "id": 7, "name": "Label E: Keringen en beschermingszones", "type": "Raster Layer", "description": "

Deze kaart toont de locaties van de beschermingzones, primaire keringen en regionale keringen binnen de Rpovincie Noord-Holland. Beschermingzone is een in de legger vastgelegde zone aan weerszijden van een waterkerende constructie waarin minder ontwikkelingen zijn toegestaan. <\/SPAN><\/P>

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Deze kaart toont de locaties van de beschermingzones, primaire keringen en regionale keringen. Beschermingzone is een in de legger vastgelegde zone aan weerszijden van een waterkerende constructie waarin minder ontwikkelingen zijn toegestaan.<\/SPAN><\/SPAN><\/P>

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De Signaalkaart Klimaatadaptatie bebouwing bodemdaling is gebaseerd op verschillende onderliggende signaalkaarten voor de geschiktheid van (toekomstige) ruimtelijke ontwikkelingen. Deze kaart signaleert welke gebieden meer of minder geschikt zijn voor een beoogde functie. In de signaalkaarten is de relatie gelegd tussen het huidige bodem en watersysteem, klimaatverandering en (toekomstig) landgebruik. De geschiktheid voor woningbouw in relatie tot de risico\u2019s voor bodemdaling is gebaseerd op de kaart Bodemdaling 2020- 2050 bij ophoging 1m zand (brondata Deltares, 2021). Deze informatie kijkt naar bodemdaling door ophoging en zetting over een langere periode. Deze kaart geeft op dit moment de beste indicatie waar en in welke mate restzetting kan worden verwacht. Gedetailleerde informatie over restzetting kan nog niet kan worden meegenomen omdat deze informatie ontbreekt. Deze kaart toont Label A: de gebieden met bodemdaling tot 3 cm. <\/SPAN><\/P>

Voor de berekeningen van de bodemdaling (2020 -205) door ophoging met 1m zand is het bodemdalingsmodel Atlantis gebruikt. Het model berekent de consolidatie en kruip over een periode van 30 jaar als gevolg van de ophoging. Veenafbraak is niet meegenomen in deze berekeningen. De ophoging drukt het veen namelijk meestal onder het grondwater of eerdere ophogingen hebben dat in het verleden al gedaan. Daarnaast heeft een ophoging zelf geen invloed op het veenafbraakproces. De bodemdalingkaart is bedoeld om inzicht te krijgen in de zettingsgevoeligheid van Nederland voor ophogingen. De randvoorwaarden van de signaalkaart bodemdaling voor bebouwing is tot stand gekomen op basis van expert judgement en samengesteld in afstemming met PNH / HHNK / AGV.<\/SPAN><\/SPAN><\/P><\/TD><\/TR>

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Voor de berekeningen van de bodemdaling (2020 -205) door ophoging met 1m zand is het bodemdalingsmodel Atlantis gebruikt. Het model berekent de consolidatie en kruip over een periode van 30 jaar als gevolg van de ophoging. Veenafbraak is niet meegenomen in deze berekeningen. De ophoging drukt het veen namelijk meestal onder het grondwater of eerdere ophogingen hebben dat in het verleden al gedaan. Daarnaast heeft een ophoging zelf geen invloed op het veenafbraakproces. De bodemdalingkaart is bedoeld om inzicht te krijgen in de zettingsgevoeligheid van Nederland voor ophogingen. De randvoorwaarden van de signaalkaart bodemdaling voor bebouwing is tot stand gekomen op basis van expert judgement en samengesteld in afstemming met PNH / HHNK / AGV.<\/SPAN><\/SPAN><\/P><\/TD><\/TR>

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Voor de berekeningen van de bodemdaling (2020 -205) door ophoging met 1m zand is het bodemdalingsmodel Atlantis gebruikt. Het model berekent de consolidatie en kruip over een periode van 30 jaar als gevolg van de ophoging. Veenafbraak is niet meegenomen in deze berekeningen. De ophoging drukt het veen namelijk meestal onder het grondwater of eerdere ophogingen hebben dat in het verleden al gedaan. Daarnaast heeft een ophoging zelf geen invloed op het veenafbraakproces. De bodemdalingkaart is bedoeld om inzicht te krijgen in de zettingsgevoeligheid van Nederland voor ophogingen. De randvoorwaarden van de signaalkaart bodemdaling voor bebouwing is tot stand gekomen op basis van expert judgement en samengesteld in afstemming met PNH / HHNK / AGV.<\/SPAN><\/SPAN><\/P><\/TD><\/TR>

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De Signaalkaart Klimaatadaptatie bebouwing bodemdaling is gebaseerd op verschillende onderliggende signaalkaarten voor de geschiktheid van (toekomstige) ruimtelijke ontwikkelingen. Deze kaart signaleert welke gebieden meer of minder geschikt zijn voor een beoogde functie. In de signaalkaarten is de relatie gelegd tussen het huidige bodem en watersysteem, klimaatverandering en (toekomstig) landgebruik. De geschiktheid voor woningbouw in relatie tot de risico\u2019s voor bodemdaling is gebaseerd op de kaart Bodemdaling 2020- 2050 bij ophoging 1m zand (brondata Deltares, 2021). Deze informatie kijkt naar bodemdaling door ophoging en zetting over een langere periode. Deze kaart geeft op dit moment de beste indicatie waar en in welke mate restzetting kan worden verwacht. Gedetailleerde informatie over restzetting kan nog niet kan worden meegenomen omdat deze informatie ontbreekt. Deze kaart toont Label D: de gebieden met bodemdaling > 90 cm. <\/SPAN><\/P>

Voor de berekeningen van de bodemdaling (2020 -205) door ophoging met 1m zand is het bodemdalingsmodel Atlantis gebruikt. Het model berekent de consolidatie en kruip over een periode van 30 jaar als gevolg van de ophoging. Veenafbraak is niet meegenomen in deze berekeningen. De ophoging drukt het veen namelijk meestal onder het grondwater of eerdere ophogingen hebben dat in het verleden al gedaan. Daarnaast heeft een ophoging zelf geen invloed op het veenafbraakproces. De bodemdalingkaart is bedoeld om inzicht te krijgen in de zettingsgevoeligheid van Nederland voor ophogingen. De randvoorwaarden van de signaalkaart bodemdaling voor bebouwing is tot stand gekomen op basis van expert judgement en samengesteld in afstemming met PNH / HHNK / AGV.<\/SPAN><\/SPAN><\/P><\/TD><\/TR>

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Voor woningbouw kan er rekening worden gehouden met risico op wateroverlast. Zo kan schade worden vermeden of zoveel mogelijk beperkt. Ontwikkelingen mogen de druk op het waterafvoersysteem niet vergroten (door het water binnen het projectgebied of polder te bergen). Ook wil de Provincie Noord-Holland inzetten op extra waterberging om het water afvoersysteem niet verder te belasten. Daarbij is het belangrijk om de 10% laagste oppervlaktes van polders voor waterberging te reserveren, of waterbergingsgebieden aan te wijzen. De randvoorwaarden van deze kaart zijn hierop gebaseerd.<\/SPAN><\/P>

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Uittredend grondwater heet kwel. Kwel beperkt zich doorgaans tot diepe polders en de lage randen van heuvels, duinen en plateaus. Het stroomt daar naartoe vanuit hoger gelegen gebieden, waar het water in de grond infiltreert. Infiltratie is het indringen van water in de grond. Hoogteverschillen en de bodemopbouw zorgen voor een wisselwerking tussen kwel en infiltratie. Door menselijk ingrijpen kan de 'flux' tussen kwel en infiltratie veranderen. Bijvoorbeeld door grondwaterwinningen of door maatregelen langs dijken ivm zogeheten dijkskwel bij een hoge rivierwaterstand. Kwel kan nadelig zijn voor de kwaliteit van oppervlakte, bijvoorbeeld door zout of nutriënten. Kwel kan ook van zeer goede kwaliteit zijn, zoals het water dat aan de rand van de Veluwe uittreedt.<\/SPAN><\/SPAN><\/P>

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Uittredend grondwater heet kwel. Kwel beperkt zich doorgaans tot diepe polders en de lage randen van heuvels, duinen en plateaus. Het stroomt daar naartoe vanuit hoger gelegen gebieden, waar het water in de grond infiltreert. Infiltratie is het indringen van water in de grond. Hoogteverschillen en de bodemopbouw zorgen voor een wisselwerking tussen kwel en infiltratie. Door menselijk ingrijpen kan de 'flux' tussen kwel en infiltratie veranderen. Bijvoorbeeld door grondwaterwinningen of door maatregelen langs dijken ivm zogeheten dijkskwel bij een hoge rivierwaterstand. Kwel kan nadelig zijn voor de kwaliteit van oppervlakte, bijvoorbeeld door zout of nutriënten. Kwel kan ook van zeer goede kwaliteit zijn, zoals het water dat aan de rand van de Veluwe uittreedt.<\/SPAN><\/P>

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Selectie van gebieden met 10% laagste gebieden van polders. Reserveer ten minste 10% van de laagste delen van polders voor waterberging. Zet in op extra waterberging om het waterafvoersysteem niet verder te belasten. Dit kan in laaggelegen gebieden binnen polders waar het water zich van nature verzameld, of door de aanleg van waterbergingsgebieden.. Zet in op nattere teelten, extensivering van de landbouw, andere gewasrotaties en zie multifunctionele waterberging (bv in combinatie met recreatie / energieopwekking) als een kans. In deze gebieden kan waterbestendig worden ontwikkeld.<\/SPAN><\/P>

Label C - Reserveer ten minste 10% van de laagste delen van polders voor waterberging. Zet om het waterafvoersysteem niet verder te belasten in op extra waterberging. Dit kan in laaggelegen gebieden binnen polders waar het water zich van nature verzameld, of door de aanleg van waterbergingsgebieden. In deze gebieden kan waterbestendig worden ontwikkeld.<\/SPAN><\/P>

deze data mag alleen worden gebruikt voor het project signaalkaart klimaatadaptatie<\/SPAN><\/SPAN><\/P><\/DIV><\/DIV><\/DIV>", "geometryType": null, "copyrightText": "", "parentLayer": { "id": 19, "name": "Wateroverlast" }, "subLayers": [], "minScale": 0, "maxScale": 0, "defaultVisibility": false, "extent": { "xmin": 94111.9235, "ymin": 464252.60829999996, "xmax": 150056.9235, "ymax": 577772.6083, "spatialReference": { "wkid": 28992, "latestWkid": 28992, "xyTolerance": 0.001, "zTolerance": 0.001, "mTolerance": 0.001, "falseX": -30515500, "falseY": -30279500, "xyUnits": 10000, "falseZ": -100000, "zUnits": 10000, "falseM": -100000, "mUnits": 10000 } }, "hasAttachments": false, "htmlPopupType": "esriServerHTMLPopupTypeNone", "displayField": "Value", "typeIdField": null, "subtypeFieldName": null, "subtypeField": null, "defaultSubtypeCode": null, "fields": [ { "name": "objectid", "type": "esriFieldTypeOID", "alias": "objectid", "domain": null }, { "name": "value", "type": "esriFieldTypeInteger", "alias": "value", "domain": null }, { "name": "count", "type": "esriFieldTypeDouble", "alias": "count", "domain": null } ], "geometryField": {}, "indexes": [ { "name": "r4022_sde_rowid_uk", "fields": "objectid", "isAscending": true, "isUnique": true, "description": "" } ], "subtypes": [], "relationships": [], "canModifyLayer": false, "canScaleSymbols": false, "hasLabels": false, "capabilities": "Map,Query", "supportsStatistics": false, "supportsExceedsLimitStatistics": false, "supportsAdvancedQueries": false, "supportedQueryFormats": "JSON, geoJSON, PBF", "isDataVersioned": false, "ownershipBasedAccessControlForFeatures": {"allowOthersToQuery": true}, "useStandardizedQueries": true, "advancedQueryCapabilities": { "useStandardizedQueries": true, "supportsStatistics": false, "supportsPercentileStatistics": false, "supportsHavingClause": false, "supportsOrderBy": false, "supportsDistinct": false, "supportsCountDistinct": false, "supportsAdvancedQueryRelated": true, "supportsQueryRelatedPagination": true, "supportsPagination": false, "supportsLod": false, "supportsQueryWithLodSR": false, "supportsTrueCurve": true, "supportsQueryWithDatumTransformation": true, "supportsReturningQueryExtent": true, "supportsQueryWithDistance": true, "supportsSqlExpression": false, "supportsTimeRelation": true, "supportsSqlFormat": false, "supportsQueryAnalytic": false, "supportsCurrentUserQueries": true }, "supportsDatumTransformation": true, "dateFieldsTimeReference": null, "preferredTimeReference": null, "datesInUnknownTimezone": false, "hasMetadata": true, "isDataArchived": false, "archivingInfo": { "supportsQueryWithHistoricMoment": false, "startArchivingMoment": -1 }, "supportsCoordinatesQuantization": true, "supportsDynamicLegends": true }, { "currentVersion": 11.3, "cimVersion": "3.3.0", "id": 20, "name": "Label C: Zoekgebieden vernatting", "type": "Raster Layer", "description": "

Zet in op extensievere vormen van landbouw en aangepaste teelten in gebieden met een beperkte drooglegging. Intensievere vormen van landbouw zullen in de toekomst niet meer houdbaar zijn in veengebieden vanwege het verhoogde grondwaterpeil tot 20 - 40 cm onder maaiveld (brief Water en Bodem sturend). Er is lokaal maatwerk nodig om gezamenlijk tot een landbouwtransitie te komen.<\/SPAN><\/SPAN><\/P>

Ontwikkel waterneutraal (of positief) in gebieden die gevoelig zijn voor wateroverlast. In veengebieden die worden vernat ten behoeve van de reductie van CO2 uitstoot en bodemdaling, neemt de drooglegging af (en de toe). Zorg dat ontwikkelingen in deze gebieden de druk op het waterafvoersysteem (ook in de toekomst) niet vergroten door extra bergingsruimte te reserveren binnen de gebiedsontwikkeling.<\/SPAN><\/SPAN><\/P>

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Label C - Zoekgebieden vernatting bebouwing - Ontwikkel waterneutraal (of positief) in gebieden die gevoelig zijn voor wateroverlast. In veengebieden die worden vernat ten behoeve van de reductie van CO2 uitstoot en bodemdaling, neemt de drooglegging af (en de toe). 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\"De Signaalkaart Klimaatadaptatie bebouwing hitte is gebaseerd op verschillende onderliggende signaalkaarten voor de geschiktheid van (toekomstige) ruimtelijke ontwikkelingen. Deze kaart signaleert welke gebieden meer of minder geschikt zijn voor een beoogde functie. In de signaalkaarten is de relatie gelegd tussen het huidige bodem en watersysteem, klimaatverandering en (toekomstig) landgebruik. <\/SPAN><\/P>

Grootschalige bodemafdekking voor woningbouw, industrie en infrastructuur veroorzaakt hittestress. Met name in sterk versteend en stedelijk gebied kan dit leiden tot verhoogde hittestress. Dit brengt gezondheidsrisico\u2019s met zich mee voor (kwetsbare) bevolkingsgroepen en natuur. De signaalkaart hitte voor bebouwing is gebaseerd op het stedelijk hitte eiland effect. Deze kaartlaag laat het temperatuurverschil zien tussen de stad en het platteland in Nederland. \"<\/SPAN><\/P>

Deze kaart is gemaakt op basis van het stedelijk hitte eiland effect (Rijksinstituut voor Volksgezondheid en Milieu (RIVM), 2020. Beschikbaargesteld via Klimaateffectalas (dec 2021) en Atlas Natuurlijk Kapitaal.<\/SPAN><\/P><\/TD><\/TR>

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\"De Signaalkaart Klimaatadaptatie bebouwing hitte is gebaseerd op verschillende onderliggende signaalkaarten voor de geschiktheid van (toekomstige) ruimtelijke ontwikkelingen. Deze kaart signaleert welke gebieden meer of minder geschikt zijn voor een beoogde functie. In de signaalkaarten is de relatie gelegd tussen het huidige bodem en watersysteem, klimaatverandering en (toekomstig) landgebruik. <\/SPAN><\/P>

Grootschalige bodemafdekking voor woningbouw, industrie en infrastructuur veroorzaakt hittestress. Met name in sterk versteend en stedelijk gebied kan dit leiden tot verhoogde hittestress. Dit brengt gezondheidsrisico\u2019s met zich mee voor (kwetsbare) bevolkingsgroepen en natuur. De signaalkaart hitte voor bebouwing is gebaseerd op het stedelijk hitte eiland effect. Deze kaartlaag laat het temperatuurverschil zien tussen de stad en het platteland in Nederland. De kaart toont Label A: gebieden waar het temperatuurverschil minder dan 0.4 graden Celcius is tussen stad en land.\"<\/SPAN><\/P><\/TD><\/TR>

Deze kaart is gemaakt op basis van het stedelijk hitte eiland effect (Rijksinstituut voor Volksgezondheid en Milieu (RIVM), 2020. Beschikbaargesteld via Klimaateffectalas (dec 2021) en Atlas Natuurlijk Kapitaal.<\/SPAN><\/SPAN><\/P><\/TD><\/TR>

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Grootschalige bodemafdekking voor woningbouw, industrie en infrastructuur veroorzaakt hittestress. Met name in sterk versteend en stedelijk gebied kan dit leiden tot verhoogde hittestress. Dit brengt gezondheidsrisico\u2019s met zich mee voor (kwetsbare) bevolkingsgroepen en natuur. De signaalkaart hitte voor bebouwing is gebaseerd op het stedelijk hitte eiland effect. Deze kaartlaag laat het temperatuurverschil zien tussen de stad en het platteland in Nederland. De kaart toont klasse B, gebieden waar het temperatuurverschil meer dan 0.4 graden Celcius is tussen stad en land.<\/SPAN><\/P>

Deze kaart is gemaakt op basis van het stedelijk hitte eiland effect (Rijksinstituut voor Volksgezondheid en Milieu (RIVM), 2020. 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Voor woningbouw kan er rekening worden gehouden met risico op wateroverlast. Zo kan schade worden vermeden of zoveel mogelijk beperkt. Ontwikkelingen mogen de druk op het waterafvoersysteem niet vergroten (door het water binnen het projectgebied of polder te bergen). Ook wil de Provincie Noord-Holland inzetten op extra waterberging om het water afvoersysteem niet verder te belasten. Daarbij is het belangrijk om de 10% laagste oppervlaktes van polders voor waterberging te reserveren, of waterbergingsgebieden aan te wijzen. De randvoorwaarden van deze kaart zijn hierop gebaseerd.<\/SPAN><\/P>

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Deze kaart is ontwikkeld door Deltares, 2016, op basis van het Nationaal Water Model en opgenomen in de Klimaateffectatlas. Deze kaart toont waar en in welke mate kwel en infiltratie plaatsvindt. De kaart is gebaseerd op de uitkomsten van het Nationaal Water Model. Dit model geeft op landelijk niveau een beeld van de huidige situatie en verwachte ontwikkeling. Specifieke lokale factoren kunnen veel invloed hebben op grondwaterstanden en zijn niet meegenomen in deze modellering. <\/SPAN><\/P>

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Selectie van gebieden met 10% laagste gebieden van polders. Reserveer ten minste 10% van de laagste delen van polders voor waterberging. Zet in op extra waterberging om het waterafvoersysteem niet verder te belasten. Dit kan in laaggelegen gebieden binnen polders waar het water zich van nature verzameld, of door de aanleg van waterbergingsgebieden.. Zet in op nattere teelten, extensivering van de landbouw, andere gewasrotaties en zie multifunctionele waterberging (bv in combinatie met recreatie / energieopwekking) als een kans. In deze gebieden kan waterbestendig worden ontwikkeld.<\/SPAN><\/SPAN><\/P>

Label C - Reserveer ten minste 10% van de laagste delen van polders voor waterberging. Zet in op extra waterberging om het waterafvoersysteem niet verder te belasten. Hierdoor zal de natschade aan gewassen bij gelijkblijvende bedrijfsvoering / gewassenkeuze toenemen. Zet in op nattere teelten, extensivering van de landbouw, andere gewasrotaties en zie multifunctionele waterberging (bv in combinatie met recreatie / energieopwekking) als een kans. <\/SPAN><\/P>

deze data mag alleen worden gebruikt voor het project signaalkaart klimaatadaptatie<\/SPAN><\/P><\/DIV><\/DIV><\/DIV>", "geometryType": null, "copyrightText": "", "parentLayer": { "id": 28, "name": "Wateroverlast" }, "subLayers": [], "minScale": 0, "maxScale": 0, "defaultVisibility": false, "extent": { "xmin": 94111.9235, "ymin": 464252.60829999996, "xmax": 150056.9235, "ymax": 577772.6083, "spatialReference": { "wkid": 28992, "latestWkid": 28992, "xyTolerance": 0.001, "zTolerance": 0.001, "mTolerance": 0.001, "falseX": -30515500, "falseY": -30279500, "xyUnits": 10000, "falseZ": -100000, "zUnits": 10000, "falseM": -100000, "mUnits": 10000 } }, "hasAttachments": false, "htmlPopupType": "esriServerHTMLPopupTypeNone", "displayField": "Value", "typeIdField": null, "subtypeFieldName": null, "subtypeField": null, "defaultSubtypeCode": null, "fields": [ { "name": "objectid", "type": "esriFieldTypeOID", "alias": "objectid", "domain": null }, { "name": "value", "type": "esriFieldTypeInteger", "alias": "value", "domain": null }, { "name": "count", "type": "esriFieldTypeDouble", "alias": "count", "domain": null } ], "geometryField": {}, "indexes": [ { "name": "r4005_sde_rowid_uk", "fields": "objectid", "isAscending": true, "isUnique": true, "description": "" } ], "subtypes": [], "relationships": [], "canModifyLayer": false, "canScaleSymbols": false, "hasLabels": false, "capabilities": "Map,Query", "supportsStatistics": false, "supportsExceedsLimitStatistics": false, "supportsAdvancedQueries": false, "supportedQueryFormats": "JSON, geoJSON, PBF", "isDataVersioned": false, "ownershipBasedAccessControlForFeatures": {"allowOthersToQuery": true}, "useStandardizedQueries": true, "advancedQueryCapabilities": { "useStandardizedQueries": true, "supportsStatistics": false, "supportsPercentileStatistics": false, "supportsHavingClause": false, "supportsOrderBy": false, "supportsDistinct": false, "supportsCountDistinct": false, "supportsAdvancedQueryRelated": true, "supportsQueryRelatedPagination": true, "supportsPagination": false, "supportsLod": false, "supportsQueryWithLodSR": false, "supportsTrueCurve": true, "supportsQueryWithDatumTransformation": true, "supportsReturningQueryExtent": true, "supportsQueryWithDistance": true, "supportsSqlExpression": false, "supportsTimeRelation": true, "supportsSqlFormat": false, "supportsQueryAnalytic": false, "supportsCurrentUserQueries": true }, "supportsDatumTransformation": true, "dateFieldsTimeReference": null, "preferredTimeReference": null, "datesInUnknownTimezone": false, "hasMetadata": true, "isDataArchived": false, "archivingInfo": { "supportsQueryWithHistoricMoment": false, "startArchivingMoment": -1 }, "supportsCoordinatesQuantization": true, "supportsDynamicLegends": true }, { "currentVersion": 11.3, "cimVersion": "3.3.0", "id": 29, "name": "Label C: Zoekgebieden vernatting", "type": "Raster Layer", "description": "

Zet in op extensievere vormen van landbouw en aangepaste teelten in gebieden met een beperkte drooglegging. Intensievere vormen van landbouw zullen in de toekomst niet meer houdbaar zijn in veengebieden vanwege het verhoogde grondwaterpeil tot 20 - 40 cm onder maaiveld (brief Water en Bodem sturend). Er is lokaal maatwerk nodig om gezamenlijk tot een landbouwtransitie te komen.<\/SPAN><\/SPAN><\/P>

Ontwikkel waterneutraal (of positief) in gebieden die gevoelig zijn voor wateroverlast. In veengebieden die worden vernat ten behoeve van de reductie van CO2 uitstoot en bodemdaling, neemt de drooglegging af (en de toe). 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in het systeem waar zoetwater niet onder vrij verval aangevoerd kan worden" } ], "minScale": 0, "maxScale": 0, "defaultVisibility": false, "extent": { "xmin": 14758.981, "ymin": 306958.81299999997, "xmax": 276838.981, "ymax": 612558.813, "spatialReference": { "wkid": 28992, "latestWkid": 28992, "xyTolerance": 0.001, "zTolerance": 0.001, "mTolerance": 0.001, "falseX": -30515500, "falseY": -30279500, "xyUnits": 10000, "falseZ": -100000, "zUnits": 10000, "falseM": -100000, "mUnits": 10000 } }, "hasAttachments": false, "htmlPopupType": "esriServerHTMLPopupTypeNone", "displayField": "", "typeIdField": null, "subtypeFieldName": null, "subtypeField": null, "defaultSubtypeCode": null, "fields": null, "geometryField": {}, "indexes": [], "subtypes": [], "relationships": [], "canModifyLayer": false, "canScaleSymbols": false, "hasLabels": false, "capabilities": "Map,Query", "supportsStatistics": false, "supportsExceedsLimitStatistics": false, "supportsAdvancedQueries": false, 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De Signaalkaart Klimaatadaptatie landbouw droogte is gebaseerd op verschillende onderliggende signaalkaarten voor de geschiktheid van (toekomstige) ruimtelijke ontwikkelingen. Deze kaart signaleert welke gebieden meer of minder geschikt zijn voor een beoogde functie. In de signaalkaarten is de relatie gelegd tussen het huidige bodem en watersysteem, klimaatverandering en (toekomstig) landgebruik. Deze kaart geeft de geschiktheid aan voor landbouw vanuit het klimaateffect droogte. <\/SPAN><\/P><\/TD><\/TR>

Deze kaart is samengesteld op basis van de volgende brondata: Plaatsen in het systeem waar zoet water niet onder vrij verval aangevoerd kan worden, HHNK en Defacto Stedenbouw (2022), - Droogtegevoeligheid grondwaterafhankelijke natuur. KWR & FWE (2021) via Klimaateffectatlas (dec 2021) en Kaart 'Water voor terrestrische natuur' Deltares (2014) t.b.v. DANK - via Digitale Atlas Natuurlijk Kapitaal<\/SPAN><\/P><\/TD><\/TR>

<\/TD><\/TR>

<\/TD><\/TR><\/TBODY><\/TABLE>

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De Signaalkaart Klimaatadaptatie landbouw droogte is gebaseerd op verschillende onderliggende signaalkaarten voor de geschiktheid van (toekomstige) ruimtelijke ontwikkelingen. Deze kaart signaleert welke gebieden meer of minder geschikt zijn voor een beoogde functie. In de signaalkaarten is de relatie gelegd tussen het huidige bodem en watersysteem, klimaatverandering en (toekomstig) landgebruik. Deze kaart geeft de geschiktheid aan voor landbouw vanuit het klimaateffect droogte. <\/SPAN><\/P>

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De Signaalkaart Klimaatadaptatie landbouw droogte is gebaseerd op verschillende onderliggende signaalkaarten voor de geschiktheid van (toekomstige) ruimtelijke ontwikkelingen. Deze kaart signaleert welke gebieden meer of minder geschikt zijn voor een beoogde functie. In de signaalkaarten is de relatie gelegd tussen het huidige bodem en watersysteem.<\/SPAN><\/P>

Label B - Creëer zoetwaterbuffers voor natte natuur. Droogte kan onomkeerbare schade voor natuur tot gevolg hebben. De natuur kan beschermd worden door hydrologische bufferzones aan te leggen en nutriënten vanuit de landbouw in het oppervlaktewater te beperken. De hogere grondwaterstanden en een onttrekkingsverbod in deze bufferzones vragen om een aanpassing in de bedrijfsvoering of aangepaste gewastypes.<\/SPAN><\/P><\/DIV><\/DIV><\/DIV>", "geometryType": null, "copyrightText": "", "parentLayer": { "id": 34, "name": "Droogte" }, "subLayers": [], "minScale": 0, "maxScale": 0, "defaultVisibility": false, "extent": { "xmin": 14758.981, "ymin": 306958.81299999997, "xmax": 276838.981, "ymax": 612558.813, "spatialReference": { "wkid": 28992, "latestWkid": 28992, "xyTolerance": 0.001, "zTolerance": 0.001, "mTolerance": 0.001, "falseX": -30515500, "falseY": -30279500, "xyUnits": 10000, "falseZ": -100000, "zUnits": 10000, "falseM": -100000, "mUnits": 10000 } }, "hasAttachments": false, "htmlPopupType": "esriServerHTMLPopupTypeNone", "displayField": "", "typeIdField": null, "subtypeFieldName": null, "subtypeField": null, "defaultSubtypeCode": null, "fields": null, "geometryField": {}, "indexes": [], "subtypes": [], "relationships": [], "canModifyLayer": false, "canScaleSymbols": false, "hasLabels": false, "capabilities": "Map,Query", "supportsStatistics": false, "supportsExceedsLimitStatistics": false, "supportsAdvancedQueries": false, "supportedQueryFormats": "JSON, geoJSON, PBF", "isDataVersioned": false, "ownershipBasedAccessControlForFeatures": {"allowOthersToQuery": true}, "useStandardizedQueries": true, "advancedQueryCapabilities": { "useStandardizedQueries": true, "supportsStatistics": false, "supportsPercentileStatistics": false, "supportsHavingClause": false, "supportsOrderBy": false, "supportsDistinct": false, "supportsCountDistinct": false, "supportsAdvancedQueryRelated": true, "supportsQueryRelatedPagination": true, "supportsPagination": false, "supportsLod": false, "supportsQueryWithLodSR": false, "supportsTrueCurve": true, "supportsQueryWithDatumTransformation": true, "supportsReturningQueryExtent": true, "supportsQueryWithDistance": true, "supportsSqlExpression": false, "supportsTimeRelation": true, "supportsSqlFormat": false, "supportsQueryAnalytic": false, "supportsCurrentUserQueries": true }, "supportsDatumTransformation": true, "dateFieldsTimeReference": null, "preferredTimeReference": null, "datesInUnknownTimezone": false, "hasMetadata": true, "isDataArchived": false, "archivingInfo": { "supportsQueryWithHistoricMoment": false, "startArchivingMoment": -1 }, "supportsCoordinatesQuantization": true, "supportsDynamicLegends": true }, { "currentVersion": 11.3, "cimVersion": "3.3.0", "id": 35, "name": "Label C: Plaatsen in het systeem waar zoetwater niet onder vrij verval aangevoerd kan worden", "type": "Raster Layer", "description": "

De Signaalkaart Klimaatadaptatie landbouw droogte is gebaseerd op verschillende onderliggende signaalkaarten voor de geschiktheid van (toekomstige) ruimtelijke ontwikkelingen. Deze kaart signaleert welke gebieden meer of minder geschikt zijn voor een beoogde functie. In de signaalkaarten is de relatie gelegd tussen het huidige bodem en watersysteem, klimaatverandering en (toekomstig) landgebruik. Deze kaart geeft de geschiktheid aan voor landbouw vanuit het klimaateffect droogte. <\/SPAN><\/P>

Label C - In gebieden waar geen water aangevoerd kan worden vanuit het oppervlaktewatersysteem zal de landbouw zich moeten aanpassen aan steeds drogere omstandigheden (bijvoorbeeld door slim watergebruik, vasthouden water, aanpassen gewassen of bedrijfsvoering).<\/SPAN><\/P><\/DIV><\/DIV><\/DIV>", "geometryType": null, "copyrightText": "", "parentLayer": { "id": 34, "name": "Droogte" }, "subLayers": [], "minScale": 0, "maxScale": 0, "defaultVisibility": false, "extent": { "xmin": 94110.5467, "ymin": 465531.28, "xmax": 150090.5467, "ymax": 577771.28, "spatialReference": { "wkid": 28992, "latestWkid": 28992, "xyTolerance": 0.001, "zTolerance": 0.001, "mTolerance": 0.001, "falseX": -30515500, "falseY": -30279500, "xyUnits": 10000, "falseZ": -100000, "zUnits": 10000, "falseM": -100000, "mUnits": 10000 } }, "hasAttachments": false, "htmlPopupType": "esriServerHTMLPopupTypeNone", "displayField": "Value", "typeIdField": null, "subtypeFieldName": null, "subtypeField": null, 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"supportsQueryWithDistance": true, "supportsSqlExpression": false, "supportsTimeRelation": true, "supportsSqlFormat": false, "supportsQueryAnalytic": false, "supportsCurrentUserQueries": true }, "supportsDatumTransformation": true, "dateFieldsTimeReference": null, "preferredTimeReference": null, "datesInUnknownTimezone": false, "hasMetadata": true, "isDataArchived": false, "archivingInfo": { "supportsQueryWithHistoricMoment": false, "startArchivingMoment": -1 }, "supportsCoordinatesQuantization": true, "supportsDynamicLegends": false }, { "currentVersion": 11.3, "cimVersion": "3.3.0", "id": 43, "name": "Signaalkaart verzilting", "type": "Raster Layer", "description": "

Deze kaart signaleert welke gebieden meer of minder geschikt zijn voor een beoogde functie. In de signaalkaarten is de relatie gelegd tussen het huidige bodem en watersysteem, klimaatverandering en (toekomstig) landgebruik. Deze kaart geeft de geschiktheid aan voor landbouw vanuit het risico's voor verzilting. <\/SPAN><\/P>

Door zeespiegelstijging, autonome processen en bodemdaling zal het op termijn vaker voorkomen dat er langere periodes niet voldoende zoetwater beschikbaar zal zijn om de verzilting te bestrijden. De toenemende verzilting kan een veranderde doorspoelwatervraag betekenen. De verzilting brengt uitdagingen met zicht mee om de zoetwaterbeschikbaarheid in alle gebieden te blijven faciliteren. Deze kaart toont de zoutvracht naar het oppervlaktewater door bodemdaling, autonome processen e bi 1m zeespiegelstijging. Zoutvracht is de zoutconcentratie maal volumeflux grondwater in kg/ha/j. <\/SPAN><\/P>

Deze data mag alleen worden gebruikt voor het project signaalkaart klimaatadaptatie.<\/SPAN><\/P><\/DIV><\/DIV><\/DIV>", "geometryType": null, "copyrightText": "", "parentLayer": { "id": 39, "name": "Verzilting" }, "subLayers": [], "minScale": 0, "maxScale": 0, "defaultVisibility": true, "extent": { "xmin": 93000, "ymin": 464300, "xmax": 154300, "ymax": 581000, "spatialReference": { "wkid": 28992, "latestWkid": 28992, "xyTolerance": 0.001, "zTolerance": 0.001, "mTolerance": 0.001, "falseX": -30515500, "falseY": -30279500, "xyUnits": 10000, "falseZ": -100000, "zUnits": 10000, "falseM": -100000, "mUnits": 10000 } }, "hasAttachments": false, "htmlPopupType": "esriServerHTMLPopupTypeNone", "displayField": "", "typeIdField": null, "subtypeFieldName": null, "subtypeField": null, "defaultSubtypeCode": null, "fields": null, "geometryField": {}, "indexes": [], "subtypes": [], "relationships": [], "canModifyLayer": false, "canScaleSymbols": false, "hasLabels": false, "capabilities": "Map,Query", "supportsStatistics": false, "supportsExceedsLimitStatistics": false, "supportsAdvancedQueries": false, "supportedQueryFormats": "JSON, geoJSON, PBF", "isDataVersioned": false, "ownershipBasedAccessControlForFeatures": {"allowOthersToQuery": true}, "useStandardizedQueries": true, "advancedQueryCapabilities": { "useStandardizedQueries": true, "supportsStatistics": false, "supportsPercentileStatistics": false, "supportsHavingClause": false, "supportsOrderBy": false, "supportsDistinct": false, "supportsCountDistinct": false, "supportsAdvancedQueryRelated": true, "supportsQueryRelatedPagination": true, "supportsPagination": false, "supportsLod": false, "supportsQueryWithLodSR": false, "supportsTrueCurve": true, "supportsQueryWithDatumTransformation": true, "supportsReturningQueryExtent": true, "supportsQueryWithDistance": true, "supportsSqlExpression": false, "supportsTimeRelation": true, "supportsSqlFormat": false, "supportsQueryAnalytic": false, "supportsCurrentUserQueries": true }, "supportsDatumTransformation": true, "dateFieldsTimeReference": null, "preferredTimeReference": null, "datesInUnknownTimezone": false, "hasMetadata": true, "isDataArchived": false, "archivingInfo": { "supportsQueryWithHistoricMoment": false, "startArchivingMoment": -1 }, "supportsCoordinatesQuantization": true, "supportsDynamicLegends": true }, { "currentVersion": 11.3, "cimVersion": "3.3.0", "id": 42, "name": "Label A: Geen noemenswaardige verzilting", "type": "Raster Layer", "description": "

De Signaalkaart Klimaatadaptatie landbouw verzilting is gebaseerd op verschillende onderliggende signaalkaarten voor de geschiktheid van (toekomstige) ruimtelijke ontwikkelingen. Deze kaart signaleert welke gebieden meer of minder geschikt zijn voor een beoogde functie. In de signaalkaarten is de relatie gelegd tussen het huidige bodem en watersysteem, klimaatverandering en (toekomstig) landgebruik. Deze kaart geeft de geschiktheid aan voor landbouw vanuit het risico's voor verzilting. <\/SPAN><\/SPAN><\/P>

Door zeespiegelstijging, autonome processen en bodemdaling zal het op termijn vaker voorkomen dat er langere periodes niet voldoende zoetwater beschikbaar zal zijn om de verzilting te bestrijden. De toenemende verzilting kan een veranderde doorspoelwatervraag betekenen. De verzilting brengt uitdagingen met zicht mee om de zoetwaterbeschikbaarheid in alle gebieden te blijven faciliteren. Deze kaart toont de zoutvracht naar het oppervlaktewater door bodemdaling, autonome processen en bij 1m zeespiegelstijging. Zoutvracht is de zoutconcentratie maal volumeflux grondwater in kg/ha/j. <\/SPAN><\/P>

<\/P>

Label A - zoutvracht < 1000 kg/ha/j bij huidig en bij 1m zeespiegelstijging - Geen noemenswaardige verzilting.<\/SPAN><\/P>

Deze data mag alleen worden gebruikt voor het project signaalkaart klimaatadaptatie.<\/SPAN><\/P><\/DIV><\/DIV><\/DIV>", "geometryType": null, "copyrightText": "", "parentLayer": { "id": 39, "name": "Verzilting" }, "subLayers": [], "minScale": 0, "maxScale": 0, "defaultVisibility": false, "extent": { "xmin": 93000, "ymin": 464300, "xmax": 154300, "ymax": 581000, "spatialReference": { "wkid": 28992, "latestWkid": 28992, "xyTolerance": 0.001, "zTolerance": 0.001, "mTolerance": 0.001, "falseX": -30515500, "falseY": -30279500, "xyUnits": 10000, "falseZ": -100000, "zUnits": 10000, "falseM": -100000, "mUnits": 10000 } }, "hasAttachments": false, "htmlPopupType": "esriServerHTMLPopupTypeNone", "displayField": "", "typeIdField": null, "subtypeFieldName": null, "subtypeField": null, "defaultSubtypeCode": null, "fields": null, "geometryField": {}, "indexes": [], "subtypes": [], "relationships": [], "canModifyLayer": false, "canScaleSymbols": false, "hasLabels": false, "capabilities": "Map,Query", "supportsStatistics": false, "supportsExceedsLimitStatistics": false, "supportsAdvancedQueries": false, "supportedQueryFormats": "JSON, geoJSON, PBF", "isDataVersioned": false, "ownershipBasedAccessControlForFeatures": {"allowOthersToQuery": true}, "useStandardizedQueries": true, "advancedQueryCapabilities": { "useStandardizedQueries": true, "supportsStatistics": false, "supportsPercentileStatistics": false, "supportsHavingClause": false, "supportsOrderBy": false, "supportsDistinct": false, "supportsCountDistinct": false, "supportsAdvancedQueryRelated": true, "supportsQueryRelatedPagination": true, "supportsPagination": false, "supportsLod": false, "supportsQueryWithLodSR": false, "supportsTrueCurve": true, "supportsQueryWithDatumTransformation": true, "supportsReturningQueryExtent": true, "supportsQueryWithDistance": true, "supportsSqlExpression": false, "supportsTimeRelation": true, "supportsSqlFormat": false, "supportsQueryAnalytic": false, "supportsCurrentUserQueries": true }, "supportsDatumTransformation": true, "dateFieldsTimeReference": null, "preferredTimeReference": null, "datesInUnknownTimezone": false, "hasMetadata": true, "isDataArchived": false, "archivingInfo": { "supportsQueryWithHistoricMoment": false, "startArchivingMoment": -1 }, "supportsCoordinatesQuantization": true, "supportsDynamicLegends": true }, { "currentVersion": 11.3, "cimVersion": "3.3.0", "id": 40, "name": "Label C: Gebieden met interne verzilting bij 1m zeespiegelstijging", "type": "Raster Layer", "description": "

De Signaalkaart Klimaatadaptatie landbouw verzilting is gebaseerd op verschillende onderliggende signaalkaarten voor de geschiktheid van (toekomstige) ruimtelijke ontwikkelingen. Deze kaart signaleert welke gebieden meer of minder geschikt zijn voor een beoogde functie. In de signaalkaarten is de relatie gelegd tussen het huidige bodem en watersysteem, klimaatverandering en (toekomstig) landgebruik. Deze kaart geeft de geschiktheid aan voor landbouw vanuit het risico's voor verzilting. <\/SPAN><\/SPAN><\/P>

Door zeespiegelstijging, autonome processen en bodemdaling zal het op termijn vaker voorkomen dat er langere periodes niet voldoende zoetwater beschikbaar zal zijn om de verzilting te bestrijden. De toenemende verzilting kan een veranderde doorspoelwatervraag betekenen. De verzilting brengt uitdagingen met zicht mee om de zoetwaterbeschikbaarheid in alle gebieden te blijven faciliteren. Deze kaart toont de zoutvracht naar het oppervlaktewater door bodemdaling, autonome processen e bi 1m zeespiegelstijging. Zoutvracht is de zoutconcentratie maal volumeflux grondwater in kg/ha/j. <\/SPAN><\/P>

Label C - Zoutvracht > 2500 kg/ ha/j bij huidig en bij 1m zeespiegelstijging - In gebieden met sterke interne verzilting kan er in droge perioden onvoldoende water beschikbaar zijn om door te spoelen. Hou rekening met een aanpassing van de gewaskeuze of bedrijfsvoering (van met name hoogwaardige zoutgevoelige gewassen).<\/SPAN><\/P>

Deze data mag alleen worden gebruikt voor het project signaalkaart klimaatadaptatie.<\/SPAN><\/P><\/DIV><\/DIV><\/DIV>", "geometryType": null, "copyrightText": "", "parentLayer": { "id": 39, "name": "Verzilting" }, "subLayers": [], "minScale": 0, "maxScale": 0, "defaultVisibility": false, "extent": { "xmin": 93000, "ymin": 464300, "xmax": 154300, "ymax": 581000, "spatialReference": { "wkid": 28992, "latestWkid": 28992, "xyTolerance": 0.001, "zTolerance": 0.001, "mTolerance": 0.001, "falseX": -30515500, "falseY": -30279500, "xyUnits": 10000, "falseZ": -100000, "zUnits": 10000, "falseM": -100000, "mUnits": 10000 } }, "hasAttachments": false, "htmlPopupType": "esriServerHTMLPopupTypeNone", "displayField": "Value", "typeIdField": null, "subtypeFieldName": null, "subtypeField": null, "defaultSubtypeCode": null, "fields": [ { "name": "objectid", "type": "esriFieldTypeOID", "alias": "objectid", "domain": null }, { "name": "value", "type": "esriFieldTypeInteger", "alias": "value", "domain": null }, { "name": "count", "type": "esriFieldTypeDouble", "alias": "count", "domain": null } ], "geometryField": {}, "indexes": [ { "name": "r4031_sde_rowid_uk", "fields": "objectid", "isAscending": true, "isUnique": true, "description": "" } ], "subtypes": [], "relationships": [], "canModifyLayer": false, "canScaleSymbols": false, "hasLabels": false, "capabilities": "Map,Query", "supportsStatistics": false, "supportsExceedsLimitStatistics": false, "supportsAdvancedQueries": false, "supportedQueryFormats": "JSON, geoJSON, PBF", "isDataVersioned": false, "ownershipBasedAccessControlForFeatures": {"allowOthersToQuery": true}, "useStandardizedQueries": true, "advancedQueryCapabilities": { "useStandardizedQueries": true, "supportsStatistics": false, "supportsPercentileStatistics": false, "supportsHavingClause": false, "supportsOrderBy": false, "supportsDistinct": false, "supportsCountDistinct": false, "supportsAdvancedQueryRelated": true, "supportsQueryRelatedPagination": true, "supportsPagination": false, "supportsLod": false, "supportsQueryWithLodSR": false, "supportsTrueCurve": true, "supportsQueryWithDatumTransformation": true, "supportsReturningQueryExtent": true, "supportsQueryWithDistance": true, "supportsSqlExpression": false, "supportsTimeRelation": true, "supportsSqlFormat": false, "supportsQueryAnalytic": false, "supportsCurrentUserQueries": true }, "supportsDatumTransformation": true, "dateFieldsTimeReference": null, "preferredTimeReference": null, "datesInUnknownTimezone": false, "hasMetadata": true, "isDataArchived": false, "archivingInfo": { "supportsQueryWithHistoricMoment": false, "startArchivingMoment": -1 }, "supportsCoordinatesQuantization": true, "supportsDynamicLegends": true }, { "currentVersion": 11.3, "cimVersion": "3.3.0", "id": 44, "name": "Hexagonen", "type": "Feature Layer", "description": "

De kaart bevat om en nabij 3600 polygonen die het oppervlak van de Provincie bedekken. Aan elk polygon zit een attribuutwaarde (A, B, C, D, E, weergeven in cijfers op een schaal van 1 tot 5) per signaalkaart die aangeeft wat de hoogste waarde is van het desbetreffende signaal in dat specifieke hexagon. Daarnaast heeft elk hexagon een attribuut voor het desbetreffende landschapstype wat overheersend is in dat hexagon.<\/SPAN><\/SPAN><\/P>

De input voor de hexagonenkaart is een polygonenbestand met willekeurig geregenereerde hexagonen, gecombineerd met de losse rasterbestanden van de signaalkaarten. Met de zogeheten \u2018zonal statistics\u2019 in ArcGIS is voor elke signaalkaart per polygoon bepaald wat de hoogst voorkomende categorie (A, B, C, D of E) is binnen dat specifieke polygoon. Deze categorieën worden weergegeven door cijfers op een schaal van 1 tot en met 5. Als bijvoorbeeld bij de signaalkaart van Overstroming een polygoon voor 20% uit categorie A en voor 80% uit categorie D bestaat, zal dat polygoon voor het signaal Overstroming in categorie D vallen. Dit proces gebeurt voor elke signaalkaart, waardoor ieder polygoon een signaalwaarde heeft voor Bebouwing-Overstroming, Bebouwing-Wateroverlast, Bebouwing-Bodemdaling, Bebouwing-Hitte, Landbouw-Verzilting, Landbouw-Droogte en Landbouw-Overstroming. <\/SPAN><\/P>

Daarna is ook per polygoon bepaald welk landschapstype het meeste voorkomt in dat specifieke polygoon, en dat landschapstype als attribuut aan dat polygoon meegegeven<\/SPAN><\/SPAN><\/P><\/TD><\/TR>

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