Raster List
API endpoint for rasterlayer objects.
Rasterlayers visualise raster data. The actual data is contained in
rastersources. To connect a rasterlayer to a rastersource, configure the
rasterlayer's source field as follows:
{
"graph": {
"rastersource": [
"lizard_nxt.blocks.LizardRasterSource",
"<uuid of a rastersource object>"
]
},
"name": "rastersource"
}
Note that the organisations of the rastersource and rasterlayer should be
equal. The raster_sources field cannot be used to configure the source:
it is merely a (read-only) hyperlink to the /rastersources endpoint.
GeoBlocks
Instead of directly visualising a raster source, raster layers can also
perform on-the-fly operations on multiple raster sources. This can be done
by extending the above example for the source field. See
https://docs.lizard.net. Note that the rasterlayers's organisation must
have geoblocks-permissions to be able to use this feature.
Deletion
If a rasterlayer is deleted, its raster sources (see /rastersources endpoint) will remain available. These need to be cleaned up seperately, or else they will keep using space.
If a rastersource was deleted while there was a rasterlayer referencing it,
the rasterlayer will become broken. In this case, the deleted rastersources
will be listed in the source.deleted_sources field.
Query parameters:
name
Text filter on the name field. All text field filter methods,
like startswith, endswith, icontains are supported.
uuid
Filter on uuid field. UUIDs must be separated by commas and must be
specified in their canonical textual representation (in their
8-4-4-4-12 form, that is). Filtering is case insensitive and may be
done across relationships.
organisation
Filter on Organisations.
observation_type
Filter on ObservationType.
layer_collections
Filter on LayerCollection.
first_value_timestamp
Temporal filter on first_value_timestamp.
last_value_timestamp
Temporal filter on last_value_timestamp.
raster_sources__uuid
Show rasters that make use of a raster_source with given uuid.
access_modifier
Filter on access_modifier, options are 'Public', 'Private', 'Common', or 'Hidden'.
ordering
Show the results in a specific order.
You can order them by name, last_modified, supplier,
temporal, access_modifier, first_value_timestamp,
last_value_timestamp, observation_type, observation_type__code,
observation_type__parameter, observation_type__unit, and
organisation__name. Add a - in front to reverse the order.
created:
Temporal filter on created. Supports various lookup types
(exact, lt, lte, gt, gte; created__exact by default).
Filter values should be specified in ISO 8601 YYYY-MM-DDThh:mm:ssZ format.
last_modified:
Temporal filter on last_modified. Supports various lookup types
(exact, lt, lte, gt, gte; last_modified__exact by default).
Filter values should be specified in ISO 8601 YYYY-MM-DDThh:mm:ssZ format.
Examples
?name__icontains=Elevation
?organisation__name=DDSC
?organisation__uuid=61f5a464c35044c19bc7d4b42d7f58cb
?organisation__name__startswith=Nelen
?organisation__name__icontains=Schuur
?observation_type__code=HOOGTEmNAP
?observation_type__parameter=Hoogte
?uuid=10415ccb-ec31-4d43-bdb3-db597061527b,
4a544b7a-772b-45fb-9aa4-a69447f34f52
?first_value_timestamp=2016-06-21T06:05:00Z
?first_value_timestamp__lt=2016-06-21T06:05:00Z
?layer_collections__slug=10855cc
?raster_sources__uuid=10415ccb-ec31-4d43-bdb3-db597061527b
?access_modifier=Private
?access_modifier=100
?ordering=name
?ordering=-last_modified
?created__gte=2017-01-01T00:00:00Z
?last_modified__lt=2018-01-01T00:00:00Z
GET /api/v4/rasters/?format=api&page=20
{ "count": 2103, "next": "https://demo.lizard.net/api/v4/rasters/?format=api&page=21", "previous": "https://demo.lizard.net/api/v4/rasters/?format=api&page=19", "results": [ { "url": "https://demo.lizard.net/api/v4/rasters/5a578206-f487-400b-8d49-1791947e3fe8/?format=api", "uuid": "5a578206-f487-400b-8d49-1791947e3fe8", "last_modified": "2020-02-20T14:47:06.169506Z", "created": "2020-02-20T14:47:05.966261Z", "organisation": { "url": "https://demo.lizard.net/api/v4/organisations/fef9e6e0-0c30-4e8c-a8cd-4f9d8e65922a/?format=api", "uuid": "fef9e6e0-0c30-4e8c-a8cd-4f9d8e65922a", "name": "Twents Waternetwerk" }, "access_modifier": "Public", "supplier": "remo.vantilburg", "shared_with": [], "writable": false, "is_geoblock": true, "weight": 4, "name": "Hittestress door warme nachten", "description": "Deze kaart geeft een inschatting van het gemiddelde aantal tropische nachten per jaar in het stedelijk gebied. Tijdens een tropische nacht daalt de temperatuur niet onder de 20 graden Celsius. Warme nachten zijn een belangrijke factor voor hittestress.Deze kaart is gebaseerd op het WH-scenario voor 2050. Het WH scenario kent de hoogte temperaturen van de vier KNMI’14-scenario’s . In het rekenmodel is het effect van ‘hitte-eilanden’ meegenomen. In buurten met veel verharding is minder verdamping door planten, waardoor het warmer kan worden. Door de aanwezigheid van gebouwen koelt het ’s nachts ook minder snel af: de warmte blijft tussen gebouwen hangen. Hittestress kan bij kwetsbare groepen leiden tot meer arbeidsuitval, een toename van ziektes en vervroegde sterfte. Bij hittestress gaat het niet alleen om hoge temperaturen, maar ook om de combinatie met luchtverontreiniging.Voor dit kaartbeeld zijn metingen uit Rotterdam gebruikt. De onderzoeksresultaten zijn doorvertaald naar de rest van Nederland, op basis van de hoeveelheid verharding, de hoeveelheid groen en de gemiddelde gebouwhoogte.VerantwoordingDeze kaart en bijbehorende tekst zijn afkomstig uit de klimaateffectenatlas (CAS) uit 2019.", "observation_type": { "url": "https://demo.lizard.net/api/v4/observationtypes/1036/?format=api", "id": 1036, "code": "index", "parameter": "Index", "unit": "", "scale": "interval", "description": "", "domain_values": null, "reference_frame": null, "compartment": null, "created": "2019-04-03T13:10:41.085507Z", "last_modified": "2019-06-25T07:26:10.441021Z" }, "temporal": false, "layer_collections": [], "first_value_timestamp": "1970-01-01T00:00:00Z", "last_value_timestamp": "1970-01-01T00:00:00Z", "spatial_bounds": { "west": 3.2570029994009526, "east": 7.2370404726252096, "north": 53.48620016182852, "south": 50.734626564692725 }, "projection": "EPSG:28992", "origin_x": 13588.8063965096, "origin_y": 306893.819439503, "upper_bound_x": 277788.80639651, "upper_bound_y": 612693.819439503, "pixelsize_x": 100.0, "pixelsize_y": -100.0, "interval": null, "wms_info": { "endpoint": "https://demo.lizard.net/wms/", "layer": "twents-waternetwerk:hittestress-door-warme-nachten" }, "options": { "styles": "Reds:0.411:0.645" }, "rescalable": false, "aggregation_type": "curve", "dtype": null, "fill_value": null }, { "url": "https://demo.lizard.net/api/v4/rasters/63b75bc0-2fbf-45e6-8c88-8db7da68900d/?format=api", "uuid": "63b75bc0-2fbf-45e6-8c88-8db7da68900d", "last_modified": "2020-02-20T14:47:22.217077Z", "created": "2020-02-20T14:47:21.988489Z", "organisation": { "url": "https://demo.lizard.net/api/v4/organisations/fef9e6e0-0c30-4e8c-a8cd-4f9d8e65922a/?format=api", "uuid": "fef9e6e0-0c30-4e8c-a8cd-4f9d8e65922a", "name": "Twents Waternetwerk" }, "access_modifier": "Public", "supplier": "remo.vantilburg", "shared_with": [], "writable": false, "is_geoblock": true, "weight": 4, "name": "Huidig gemiddeld laagste grondwaterstand", "description": "Deze laag geeft de huidige gemiddeld laagste grondwaterstand aan in Twente volgens modelsimulaties. De gemiddeld laagste grondwaterstand is met name van belang voor natuur, landbouw en drinkwatervoorziening.VerantwoordingDe bron van deze kaart is het nationaal grondwatermodel van 2017 en de studie Zoetwatervoorziening Oost Nederland.", "observation_type": { "url": "https://demo.lizard.net/api/v4/observationtypes/521/?format=api", "id": 521, "code": "Waterdepth", "parameter": "Waterdepth", "unit": "m", "scale": "interval", "description": "interval", "domain_values": null, "reference_frame": null, "compartment": null, "created": "2016-07-14T10:07:22.899825Z", "last_modified": "2022-02-02T14:47:44.543819Z" }, "temporal": false, "layer_collections": [], "first_value_timestamp": "1970-01-01T00:00:00Z", "last_value_timestamp": "1970-01-01T00:00:00Z", "spatial_bounds": { "west": 4.943732300234112, "east": 7.097408739231976, "north": 53.03283826338092, "south": 51.81979238538452 }, "projection": "EPSG:28992", "origin_x": 125250.0, "origin_y": 427000.0, "upper_bound_x": 269750.0, "upper_bound_y": 560750.0, "pixelsize_x": 250.0, "pixelsize_y": -250.0, "interval": null, "wms_info": { "endpoint": "https://demo.lizard.net/wms/", "layer": "twents-waternetwerk:huidig-gemiddeld-laagste-grondwaterstand" }, "options": { "styles": "BluGreRed2:0:2" }, "rescalable": false, "aggregation_type": "curve", "dtype": null, "fill_value": null }, { "url": "https://demo.lizard.net/api/v4/rasters/738f4166-7bb0-49f6-ac1f-3388cde3fe3e/?format=api", "uuid": "738f4166-7bb0-49f6-ac1f-3388cde3fe3e", "last_modified": "2020-02-20T14:47:38.337794Z", "created": "2020-02-20T14:47:38.146827Z", "organisation": { "url": "https://demo.lizard.net/api/v4/organisations/fef9e6e0-0c30-4e8c-a8cd-4f9d8e65922a/?format=api", "uuid": "fef9e6e0-0c30-4e8c-a8cd-4f9d8e65922a", "name": "Twents Waternetwerk" }, "access_modifier": "Public", "supplier": "remo.vantilburg", "shared_with": [], "writable": false, "is_geoblock": true, "weight": 4, "name": "Kwel (huidig)", "description": "Deze kaart geeft de locaties en intensiteit van huidige kwel in Twente volgens modelsimulaties.VerantwoordingBron: Zoetwatervoorziening Oost Nederland (ZON) Gevolgen van droogte voor het waterbeheer, Hoofdrapport , Tauw (15 oktober 2012). Kaarten uit 2019.", "observation_type": { "url": "https://demo.lizard.net/api/v4/observationtypes/521/?format=api", "id": 521, "code": "Waterdepth", "parameter": "Waterdepth", "unit": "m", "scale": "interval", "description": "interval", "domain_values": null, "reference_frame": null, "compartment": null, "created": "2016-07-14T10:07:22.899825Z", "last_modified": "2022-02-02T14:47:44.543819Z" }, "temporal": false, "layer_collections": [], "first_value_timestamp": "1970-01-01T00:00:00Z", "last_value_timestamp": "1970-01-01T00:00:00Z", "spatial_bounds": { "west": 4.943732300234112, "east": 7.097408739231976, "north": 53.03283826338092, "south": 51.81979238538452 }, "projection": "EPSG:28992", "origin_x": 125250.0, "origin_y": 427000.0, "upper_bound_x": 269750.0, "upper_bound_y": 560750.0, "pixelsize_x": 250.0, "pixelsize_y": -250.0, "interval": null, "wms_info": { "endpoint": "https://demo.lizard.net/wms/", "layer": "twents-waternetwerk:kwel-huidig" }, "options": { "styles": "Blues_trans:-2:1.5" }, "rescalable": false, "aggregation_type": "curve", "dtype": null, "fill_value": null }, { "url": "https://demo.lizard.net/api/v4/rasters/b58e0a0e-9893-4af2-9772-2b9812d03d7f/?format=api", "uuid": "b58e0a0e-9893-4af2-9772-2b9812d03d7f", "last_modified": "2020-02-20T14:47:54.328882Z", "created": "2020-02-20T14:47:54.103122Z", "organisation": { "url": "https://demo.lizard.net/api/v4/organisations/fef9e6e0-0c30-4e8c-a8cd-4f9d8e65922a/?format=api", "uuid": "fef9e6e0-0c30-4e8c-a8cd-4f9d8e65922a", "name": "Twents Waternetwerk" }, "access_modifier": "Public", "supplier": "remo.vantilburg", "shared_with": [], "writable": false, "is_geoblock": true, "weight": 4, "name": "Laagste grondwaterstand extreem droge zomer (huidig)", "description": "De grondwaterstanden in extreem droge jaren kunnen op veel plekken verder uitzakken dan de GLG. Om een beeld te krijgen van de effecten van een extreem droog jaar op de grondwaterstand kan er in plaats van de GLG beter gekeken worden naar de laagste grondwaterstanden (LG3) voor een specifiek extreem droog jaar als 1976. Bij een te lage grondwaterstand kan schade ontstaan, bijvoorbeeld aan gewassen. Deze kaart laat de laagste grondwaterstanden (LG3) zien voor een extreem droge zomer.In landbouwgebieden waar oppervlaktewaterpeilbeheer mogelijk is, zoals in polders, wordt het bodemvocht onder normale omstandigheden aangevuld vanuit het grondwater. Bij droogte kan de grondwaterstand zo ver dalen, dat dit niet meer gebeurt. Er kan dan beregend worden of er ontstaat droogteschade.In natuurgebieden past de vegetatie zich over het algemeen aan. De schade aan de natuur bestaat uit het risico op onomkeerbare veranderingen, waarbij nattere doelsoorten verdwijnen en drogere doelsoorten het gebied niet kunnen bereiken.In het veenweidegebied wordt goed op de grondwaterstanden gelet omdat bij lagere grondwaterstanden meer veenoxidatie, CO2 uitstoot en bodemdaling plaatsvindtDe kaart is gebaseerd op de uitkomsten van het Nationaal Water Model - Basisprognoses 2018. Dit model geeft op landelijk niveau een beeld van de verwachte ontwikkeling. Specifieke lokale factoren kunnen veel invloed hebben op de grondwaterstanden en zijn niet meegenomen in deze modellering. VerantwoordingBron: CAS Klimaateffectatlas (2019).", "observation_type": { "url": "https://demo.lizard.net/api/v4/observationtypes/500/?format=api", "id": 500, "code": "Waterlevel", "parameter": "Waterlevel", "unit": "m", "scale": "interval", "description": "", "domain_values": null, "reference_frame": "MSL", "compartment": "", "created": "2016-04-26T07:35:56.545260Z", "last_modified": "2019-06-25T07:26:10.441021Z" }, "temporal": false, "layer_collections": [], "first_value_timestamp": "1970-01-01T00:00:00Z", "last_value_timestamp": "1970-01-01T00:00:00Z", "spatial_bounds": { "west": 3.253713155100211, "east": 7.243161224559517, "north": 53.54488089129097, "south": 50.73417297437435 }, "projection": "EPSG:28992", "origin_x": 13564.4, "origin_y": 306844.0, "upper_bound_x": 278026.4, "upper_bound_y": 619234.0, "pixelsize_x": 250.0, "pixelsize_y": -250.0, "interval": null, "wms_info": { "endpoint": "https://demo.lizard.net/wms/", "layer": "twents-waternetwerk:laagste-grondwaterstand-extreem-droge-zomer-" }, "options": { "styles": "BluGreRed2:0.2:2" }, "rescalable": false, "aggregation_type": "curve", "dtype": null, "fill_value": null }, { "url": "https://demo.lizard.net/api/v4/rasters/fc353860-76a6-419c-a4ae-2ab07435b897/?format=api", "uuid": "fc353860-76a6-419c-a4ae-2ab07435b897", "last_modified": "2020-02-20T14:48:11.014560Z", "created": "2020-02-20T14:48:10.785189Z", "organisation": { "url": "https://demo.lizard.net/api/v4/organisations/fef9e6e0-0c30-4e8c-a8cd-4f9d8e65922a/?format=api", "uuid": "fef9e6e0-0c30-4e8c-a8cd-4f9d8e65922a", "name": "Twents Waternetwerk" }, "access_modifier": "Public", "supplier": "remo.vantilburg", "shared_with": [], "writable": false, "is_geoblock": true, "weight": 4, "name": "Landgebruik", "description": "VerantwoordingDeze landgebruikskaart is samengesteld op basis van de volgende openbare databronnen: het BAG-register, de TOP10NL, de Basisregistratiegewaspercelen, het NWB en de BGT. Deze databronnen worden in de landgebruikskaart gecombineerd. Hierdoor is een optimaal onderscheid te maken tussen de verschillende landgebruikscategorieën.", "observation_type": { "url": "https://demo.lizard.net/api/v4/observationtypes/502/?format=api", "id": 502, "code": "KLASSE", "parameter": "Klasse", "unit": "", "scale": "nominal", "description": "", "domain_values": null, "reference_frame": "", "compartment": "", "created": "2016-04-26T07:49:44.396529Z", "last_modified": "2019-06-25T07:26:10.441021Z" }, "temporal": false, "layer_collections": [], "first_value_timestamp": "1970-01-01T00:00:00Z", "last_value_timestamp": "1970-01-01T00:00:00Z", "spatial_bounds": { "west": 3.253713155100211, "east": 7.243161224559517, "north": 53.54488089129097, "south": 50.73417297437435 }, "projection": "EPSG:28992", "origin_x": 13564.4, "origin_y": 306844.0, "upper_bound_x": 278026.4, "upper_bound_y": 619234.0, "pixelsize_x": 0.5, "pixelsize_y": -0.5, "interval": null, "wms_info": { "endpoint": "https://demo.lizard.net/wms/", "layer": "twents-waternetwerk:landgebruik" }, "options": { "styles": "lc-fun_klimaatatlas" }, "rescalable": false, "aggregation_type": "curve", "dtype": null, "fill_value": null }, { "url": "https://demo.lizard.net/api/v4/rasters/9250583c-5b41-4300-8c98-1053b3b0f8ec/?format=api", "uuid": "9250583c-5b41-4300-8c98-1053b3b0f8ec", "last_modified": "2020-02-20T14:48:26.916556Z", "created": "2020-02-20T14:48:26.703253Z", "organisation": { "url": "https://demo.lizard.net/api/v4/organisations/fef9e6e0-0c30-4e8c-a8cd-4f9d8e65922a/?format=api", "uuid": "fef9e6e0-0c30-4e8c-a8cd-4f9d8e65922a", "name": "Twents Waternetwerk" }, "access_modifier": "Public", "supplier": "remo.vantilburg", "shared_with": [], "writable": false, "is_geoblock": true, "weight": 4, "name": "Overstromingsdiepte buitendijksegebieden", "description": "Deze kaart laat zien welke buitendijkse gebieden overstromen bij een waterstand die een kans van voorkomen heeft van 1 keer in de 1000 jaar. Buitendijkse gebieden zijn veelal hooggelegen, onbeschermde gebieden langs de grote rivieren, meren en de kust. Deze kaart bevat de gegevens zoals gerapporteerd voor de Europese Richtlijn Overstromingsrisico's (ROR, 2013) nodig.Verantwoording Deze kaart en bijbehorende tekst zijn afkomstig uit de klimaateffectenatlas (CAS) uit 2019.", "observation_type": { "url": "https://demo.lizard.net/api/v4/observationtypes/521/?format=api", "id": 521, "code": "Waterdepth", "parameter": "Waterdepth", "unit": "m", "scale": "interval", "description": "interval", "domain_values": null, "reference_frame": null, "compartment": null, "created": "2016-07-14T10:07:22.899825Z", "last_modified": "2022-02-02T14:47:44.543819Z" }, "temporal": false, "layer_collections": [], "first_value_timestamp": "1970-01-01T00:00:00Z", "last_value_timestamp": "1970-01-01T00:00:00Z", "spatial_bounds": { "west": 3.253713155100211, "east": 7.243161224559517, "north": 53.54488089129097, "south": 50.73417297437435 }, "projection": "EPSG:28992", "origin_x": 13564.4, "origin_y": 306844.0, "upper_bound_x": 278026.4, "upper_bound_y": 619234.0, "pixelsize_x": 100.0, "pixelsize_y": -100.0, "interval": null, "wms_info": { "endpoint": "https://demo.lizard.net/wms/", "layer": "twents-waternetwerk:overstromingsdiepte-buitendijksegebieden" }, "options": { "styles": "Blues:0.1:2.77" }, "rescalable": false, "aggregation_type": "curve", "dtype": null, "fill_value": null }, { "url": "https://demo.lizard.net/api/v4/rasters/cd4fd62a-5947-4b0c-bdb2-d4c748ec00ea/?format=api", "uuid": "cd4fd62a-5947-4b0c-bdb2-d4c748ec00ea", "last_modified": "2020-02-20T14:48:42.671820Z", "created": "2020-02-20T14:48:42.491398Z", "organisation": { "url": "https://demo.lizard.net/api/v4/organisations/fef9e6e0-0c30-4e8c-a8cd-4f9d8e65922a/?format=api", "uuid": "fef9e6e0-0c30-4e8c-a8cd-4f9d8e65922a", "name": "Twents Waternetwerk" }, "access_modifier": "Public", "supplier": "remo.vantilburg", "shared_with": [], "writable": false, "is_geoblock": true, "weight": 4, "name": "Overstromingsdiepte regionale keringen", "description": "Deze kaart laat zien welke gebieden kunnen overstromen en welke overstromingsdiepte maximaal op kan treden bij een overstroming vanuit de secundaire keringen. Ofwel, het regionale watersysteem. De overstromingsdiepte speelt een rol bij de mogelijkheden voor gevolgbeperkende maatregelen en eventuele (verticale) evacuatie. De overstromingsscenario’s op deze kaart kunnen niet gelijktijdig optreden. Deze kaart bevat de gegevens zoals gerapporteerd voor de ROR in het kader van de Europese Richtlijn Overstromingsrisico’s (2013). Deze kaart is echter niet compleet omdat niet alle gebieden die vanuit het regionale systeem kunnen overstromen, hoefden te worden gerapporteerd. De lokale waterbeheerder kan een compleet beeld van deze overstromingsgevoelige gebieden beschikbaar stellen.De risico’s van overige keringen (zoals keringen van omleidingskanaaal, buursebeek, beneden Dinkel) worden op deze kaart niet getoond.VerantwoordingDeze kaart en bijbehorende tekst zijn afkomstig uit de klimaateffectenatlas (CAS) uit 2019.", "observation_type": { "url": "https://demo.lizard.net/api/v4/observationtypes/521/?format=api", "id": 521, "code": "Waterdepth", "parameter": "Waterdepth", "unit": "m", "scale": "interval", "description": "interval", "domain_values": null, "reference_frame": null, "compartment": null, "created": "2016-07-14T10:07:22.899825Z", "last_modified": "2022-02-02T14:47:44.543819Z" }, "temporal": false, "layer_collections": [], "first_value_timestamp": "1970-01-01T00:00:00Z", "last_value_timestamp": "1970-01-01T00:00:00Z", "spatial_bounds": { "west": 3.253713155100211, "east": 7.243161224559517, "north": 53.50394737221648, "south": 50.756344989396794 }, "projection": "EPSG:28992", "origin_x": 13564.4, "origin_y": 309900.0, "upper_bound_x": 278026.4, "upper_bound_y": 615000.0, "pixelsize_x": 100.0, "pixelsize_y": -100.0, "interval": null, "wms_info": { "endpoint": "https://demo.lizard.net/wms/", "layer": "twents-waternetwerk:overstromingsdiepte-regionale-keringen" }, "options": { "styles": "Blues:0.0936:2.43" }, "rescalable": false, "aggregation_type": "curve", "dtype": null, "fill_value": null }, { "url": "https://demo.lizard.net/api/v4/rasters/3c875669-0b94-4d94-935f-d42f345a9a53/?format=api", "uuid": "3c875669-0b94-4d94-935f-d42f345a9a53", "last_modified": "2020-02-20T14:48:58.486947Z", "created": "2020-02-20T14:48:58.278357Z", "organisation": { "url": "https://demo.lizard.net/api/v4/organisations/fef9e6e0-0c30-4e8c-a8cd-4f9d8e65922a/?format=api", "uuid": "fef9e6e0-0c30-4e8c-a8cd-4f9d8e65922a", "name": "Twents Waternetwerk" }, "access_modifier": "Public", "supplier": "remo.vantilburg", "shared_with": [], "writable": false, "is_geoblock": true, "weight": 4, "name": "Verandering gemiddeld hoogste grondwaterstand (WH2050)", "description": "In het KNMI WH 2050 scenario stijgt de temperatuur sterk. Door de sterke temperatuurstijging zal naar er naar verwachting meer verdamping plaatsvinden. Dit heeft implicaties voor de grondwaterstand.Deze laag geeft de procentuele verandering van de grondwaterstand in 2050 ten opzicht van de huidige situatie. De mate van de afname verschilt per locatie.KNMI scenario 2050 <a href=\"https://www.knmi.nl/kennis-en-datacentrum/uitleg/klimaatscenario-s\" title=\"https://www.knmi.nl/kennis-en-datacentrum/uitleg/klimaatscenario-s\">https://www.knmi.nl/kennis-en-datacentrum/uitleg/klimaatscenario-sVerantwoordingBron: Zoetwatervoorziening Oost Nederland (ZON) Gevolgen van droogte voor het waterbeheer, Hoofdrapport , Tauw (15 oktober 2019)", "observation_type": { "url": "https://demo.lizard.net/api/v4/observationtypes/521/?format=api", "id": 521, "code": "Waterdepth", "parameter": "Waterdepth", "unit": "m", "scale": "interval", "description": "interval", "domain_values": null, "reference_frame": null, "compartment": null, "created": "2016-07-14T10:07:22.899825Z", "last_modified": "2022-02-02T14:47:44.543819Z" }, "temporal": false, "layer_collections": [], "first_value_timestamp": "1970-01-01T00:00:00Z", "last_value_timestamp": "1970-01-01T00:00:00Z", "spatial_bounds": { "west": 4.943732300234112, "east": 7.097408739231976, "north": 53.03283826338092, "south": 51.81979238538452 }, "projection": "EPSG:28992", "origin_x": 125250.0, "origin_y": 427000.0, "upper_bound_x": 269750.0, "upper_bound_y": 560750.0, "pixelsize_x": 250.0, "pixelsize_y": -250.0, "interval": null, "wms_info": { "endpoint": "https://demo.lizard.net/wms/", "layer": "twents-waternetwerk:verandering-gemiddeld-hoogste-grondwaterstan" }, "options": { "styles": "RdBu:-0.8:0.8" }, "rescalable": false, "aggregation_type": "curve", "dtype": null, "fill_value": null }, { "url": "https://demo.lizard.net/api/v4/rasters/a0aba84b-8d29-4be2-9a2b-835697d6c202/?format=api", "uuid": "a0aba84b-8d29-4be2-9a2b-835697d6c202", "last_modified": "2020-02-20T14:49:14.282300Z", "created": "2020-02-20T14:49:14.098447Z", "organisation": { "url": "https://demo.lizard.net/api/v4/organisations/fef9e6e0-0c30-4e8c-a8cd-4f9d8e65922a/?format=api", "uuid": "fef9e6e0-0c30-4e8c-a8cd-4f9d8e65922a", "name": "Twents Waternetwerk" }, "access_modifier": "Public", "supplier": "remo.vantilburg", "shared_with": [], "writable": false, "is_geoblock": true, "weight": 4, "name": "Verandering gemiddeld laagste grondwaterstand (WH2050)", "description": "In het KNMI WH 2050 scenario stijgt de temperatuur sterk. Door de sterke temperatuurstijging zal naar er naar verwachting meer verdamping plaatsvinden. Dit heeft implicaties voor de grondwaterstand.Deze laag geeft de procentuele verandering van de grondwaterstand in 2050 ten opzicht van de huidige situatie. De mate van de afname verschilt per locatie.KNMI scenario 2050 <a href=\"https://www.knmi.nl/kennis-en-datacentrum/uitleg/klimaatscenario-s\" title=\"https://www.knmi.nl/kennis-en-datacentrum/uitleg/klimaatscenario-s\">https://www.knmi.nl/kennis-en-datacentrum/uitleg/klimaatscenario-sVerantwoordingBron: Zoetwatervoorziening Oost Nederland (ZON) Gevolgen van droogte voor het waterbeheer, Hoofdrapport , Tauw (15 oktober 2012). Kaarten uit 2019.", "observation_type": { "url": "https://demo.lizard.net/api/v4/observationtypes/521/?format=api", "id": 521, "code": "Waterdepth", "parameter": "Waterdepth", "unit": "m", "scale": "interval", "description": "interval", "domain_values": null, "reference_frame": null, "compartment": null, "created": "2016-07-14T10:07:22.899825Z", "last_modified": "2022-02-02T14:47:44.543819Z" }, "temporal": false, "layer_collections": [], "first_value_timestamp": "1970-01-01T00:00:00Z", "last_value_timestamp": "1970-01-01T00:00:00Z", "spatial_bounds": { "west": 4.943732300234112, "east": 7.097408739231976, "north": 53.03283826338092, "south": 51.81979238538452 }, "projection": "EPSG:28992", "origin_x": 125250.0, "origin_y": 427000.0, "upper_bound_x": 269750.0, "upper_bound_y": 560750.0, "pixelsize_x": 250.0, "pixelsize_y": -250.0, "interval": null, "wms_info": { "endpoint": "https://demo.lizard.net/wms/", "layer": "twents-waternetwerk:verandering-gemiddeld-laagste-grondwaterstan" }, "options": { "styles": "RdBu:-0.8:0.8" }, "rescalable": false, "aggregation_type": "curve", "dtype": null, "fill_value": null }, { "url": "https://demo.lizard.net/api/v4/rasters/1b613e55-626b-4c4e-bdca-2e6a8e86c02b/?format=api", "uuid": "1b613e55-626b-4c4e-bdca-2e6a8e86c02b", "last_modified": "2020-02-20T14:49:30.151512Z", "created": "2020-02-20T14:49:29.946085Z", "organisation": { "url": "https://demo.lizard.net/api/v4/organisations/fef9e6e0-0c30-4e8c-a8cd-4f9d8e65922a/?format=api", "uuid": "fef9e6e0-0c30-4e8c-a8cd-4f9d8e65922a", "name": "Twents Waternetwerk" }, "access_modifier": "Public", "supplier": "remo.vantilburg", "shared_with": [], "writable": false, "is_geoblock": true, "weight": 4, "name": "Verandering kwel (WH2050)", "description": "Deze kaart geeft de procentuele verandering van huidige kwel ten opzichte van de geschatte kwel in het 2050WH scenario.VerantwoordingBron: Zoetwatervoorziening Oost Nederland (ZON) Gevolgen van droogte voor het waterbeheer, Hoofdrapport , Tauw (15 oktober 2012). Kaarten uit 2019.", "observation_type": { "url": "https://demo.lizard.net/api/v4/observationtypes/521/?format=api", "id": 521, "code": "Waterdepth", "parameter": "Waterdepth", "unit": "m", "scale": "interval", "description": "interval", "domain_values": null, "reference_frame": null, "compartment": null, "created": "2016-07-14T10:07:22.899825Z", "last_modified": "2022-02-02T14:47:44.543819Z" }, "temporal": false, "layer_collections": [], "first_value_timestamp": "1970-01-01T00:00:00Z", "last_value_timestamp": "1970-01-01T00:00:00Z", "spatial_bounds": { "west": 4.943732300234112, "east": 7.097408739231976, "north": 53.03283826338092, "south": 51.81979238538452 }, "projection": "EPSG:28992", "origin_x": 125250.0, "origin_y": 427000.0, "upper_bound_x": 269750.0, "upper_bound_y": 560750.0, "pixelsize_x": 250.0, "pixelsize_y": -250.0, "interval": null, "wms_info": { "endpoint": "https://demo.lizard.net/wms/", "layer": "twents-waternetwerk:verandering-kwel-wh2050" }, "options": { "styles": "RedWhiBlu:-1:1" }, "rescalable": false, "aggregation_type": "curve", "dtype": null, "fill_value": null } ] }