{ "currentVersion": 10.91, "cimVersion": "2.9.0", "serviceDescription": "
The 12-month scale Drought Severity Index (DSI-12) was used. It is based on cumulative monthly precipitation anomalies, where the absolute deficit (in mm) is divided by the mean annual rainfall and multiplied by 100. DSI-12 is a rainfall index and therefore does not account for an increase in drought due to increasing temperatures (and subsequently potential evaporation). The map shows the ratio of the maximum DSI-12 in the future to the maximum DSI-12 in the historical period. Based on 50 climate model projections from the Coupled Model Intercomparison Project Phase 5 (CMIP5; (Taylor et al., 2012), under the RCP8.5 climate scenario.<\/SPAN><\/SPAN><\/P><\/DIV><\/DIV><\/DIV>",
"mapName": "Change factor of maximum drought between 1951-2000 and 2051-2100",
"description": "The 12-month scale Drought Severity Index (DSI-12) was used. It is based on cumulative monthly precipitation anomalies, where the absolute deficit (in mm) is divided by the mean annual rainfall and multiplied by 100. DSI-12 is a rainfall index and therefore does not account for an increase in drought due to increasing temperatures (and subsequently potential evaporation). The map shows the ratio of the maximum DSI-12 in the future to the maximum DSI-12 in the historical period. Based on 50 climate model projections from the Coupled Model Intercomparison Project Phase 5 (CMIP5; (Taylor et al., 2012), under the RCP8.5 climate scenario. ",
"copyrightText": "Guerreiro, S. B., et al., 2018, \u2018Future heat-waves, droughts and floods in 571 European cities\u2019, Environmental Research Letters 13(3), p. 034009 (DOI: 10.1088/1748-9326/aaaad3).",
"supportsDynamicLayers": true,
"layers": [
{
"id": 0,
"name": "Low impact scenario (10th percentile)",
"parentLayerId": -1,
"defaultVisibility": true,
"subLayerIds": null,
"minScale": 0,
"maxScale": 0,
"type": "Feature Layer",
"geometryType": "esriGeometryPoint",
"supportsDynamicLegends": true
},
{
"id": 1,
"name": "Medium impact scenario (50th percentile)",
"parentLayerId": -1,
"defaultVisibility": true,
"subLayerIds": null,
"minScale": 0,
"maxScale": 0,
"type": "Feature Layer",
"geometryType": "esriGeometryPoint",
"supportsDynamicLegends": true
},
{
"id": 2,
"name": "High impact scenario (90th percentile)",
"parentLayerId": -1,
"defaultVisibility": true,
"subLayerIds": null,
"minScale": 0,
"maxScale": 0,
"type": "Feature Layer",
"geometryType": "esriGeometryPoint",
"supportsDynamicLegends": true
}
],
"tables": [],
"spatialReference": {
"wkid": 102100,
"latestWkid": 3857,
"xyTolerance": 0.001,
"zTolerance": 0.001,
"mTolerance": 0.001,
"falseX": -20037700,
"falseY": -30241100,
"xyUnits": 1.4892314192838538E8,
"falseZ": -100000,
"zUnits": 10000,
"falseM": -100000,
"mUnits": 10000
},
"singleFusedMapCache": false,
"initialExtent": {
"xmin": -2770813.2736297706,
"ymin": 6320808.021129249,
"xmax": 5440477.747129772,
"ymax": 1.130115272791001E7,
"spatialReference": {
"wkid": 102100,
"latestWkid": 3857,
"xyTolerance": 0.001,
"zTolerance": 0.001,
"mTolerance": 0.001,
"falseX": -20037700,
"falseY": -30241100,
"xyUnits": 1.4892314192838538E8,
"falseZ": -100000,
"zUnits": 10000,
"falseM": -100000,
"mUnits": 10000
}
},
"fullExtent": {
"xmin": -1044275.5639999993,
"ymin": 4118270.5491999984,
"xmax": 3713940.0375000015,
"ymax": 1.0959110719400004E7,
"spatialReference": {
"wkid": 102100,
"latestWkid": 3857,
"xyTolerance": 0.001,
"zTolerance": 0.001,
"mTolerance": 0.001,
"falseX": -20037700,
"falseY": -30241100,
"xyUnits": 1.4892314192838538E8,
"falseZ": -100000,
"zUnits": 10000,
"falseM": -100000,
"mUnits": 10000
}
},
"datesInUnknownTimezone": false,
"minScale": 0,
"maxScale": 0,
"units": "esriMeters",
"supportedImageFormatTypes": "PNG32,PNG24,PNG,JPG,DIB,TIFF,EMF,PS,PDF,GIF,SVG,SVGZ,BMP",
"documentInfo": {
"Title": "Change factor of maximum drought in 571 European cities between 1951-2000 and 2051-2100.",
"Author": "",
"Comments": " The 12-month scale Drought Severity Index (DSI-12) was used. It is based on cumulative monthly precipitation anomalies, where the absolute deficit (in mm) is divided by the mean annual rainfall and multiplied by 100. DSI-12 is a rainfall index and therefore does not account for an increase in drought due to increasing temperatures (and subsequently potential evaporation). The map shows the ratio of the maximum DSI-12 in the future to the maximum DSI-12 in the historical period. Based on 50 climate model projections from the Coupled Model Intercomparison Project Phase 5 (CMIP5; (Taylor et al., 2012), under the RCP8.5 climate scenario.<\/SPAN><\/SPAN><\/P><\/DIV><\/DIV><\/DIV>",
"Subject": "The map shows the projected change in the maximum droughts experienced by cities.",
"Category": "",
"AntialiasingMode": "None",
"TextAntialiasingMode": "Force",
"Version": "10.1",
"Keywords": "climate change; cities; drought; adaptation"
},
"capabilities": "Map,Query,Data",
"supportedQueryFormats": "JSON, geoJSON, PBF",
"exportTilesAllowed": false,
"referenceScale": 0.0,
"supportsDatumTransformation": true,
"archivingInfo": {"supportsHistoricMoment": false},
"supportsClipping": true,
"supportsSpatialFilter": true,
"supportsTimeRelation": true,
"supportsQueryDataElements": true,
"maxRecordCount": 1000,
"maxImageHeight": 4096,
"maxImageWidth": 4096,
"supportedExtensions": "KmlServer, WFSServer, WMSServer"
}