Output interpretation

An explanation and interpretation of every feature outputted in the API response.

Energy & object data features

Feature	Example	Explanation
BagID	0575010000034068	VBO ID from BAG registry
PostCode	2771DS	Postcode
HouseNumber	87	House number
HouseNumberAddition	A	Addition to house number
PandID	0575100000034238	ID of the building
City	Boskoop	City name
Street	Zuidkade	Street name
BuildingStatus	Pand in gebruik	Status of the building
ObjectFunction	woonfunctie	Function of the house
InnerSurfaceArea	131	Square meters livable space
BuildYear	1961	Construction year
Monument	no	If it's a monument or not
MonumentDescription	Geen monument / Onbekend	Description of the monument
EpcLabel	B	Energy label. Possible values: "A+++++", "A++++", "A+++","A++","A+","A", "B", "C", "D", "E", "F", "G"
CalculationMethod	Rekenmethodiek Definitief Energielabel, versie 1.2, 16 september 2014	Method used for determining energy efficiency
RegistrationDate	20170814	The date when the energy label registered
Validity	20270814	The date until when the energy label is valid
PrimaryEnergyDemand	255	primary fossile energy demand expressed in kWh/m² per year (BENG2)
PercentageRenewable	17,2	% of energy coming from renewable sources
HeatDemand	181	heat demand expressed in kWh/m² per year
EnergyDemand	182	primary energy demand expressed in kWh/m² per year

Feature

Example

Explanation

BagID

0575010000034068

VBO ID from BAG registry

PostCode

2771DS

Postcode

HouseNumber

House number

HouseNumberAddition

Addition to house number

PandID

0575100000034238

ID of the building

City

Boskoop

City name

Street

Zuidkade

Street name

BuildingStatus

Pand in gebruik

Status of the building

ObjectFunction

woonfunctie

Function of the house

InnerSurfaceArea

131

Square meters livable space

BuildYear

1961

Construction year

Monument

If it's a monument or not

MonumentDescription

Geen monument / Onbekend

Description of the monument

EpcLabel

Energy label. Possible values: "A+++++", "A++++", "A+++","A++","A+","A", "B", "C", "D", "E", "F", "G"

CalculationMethod

Rekenmethodiek Definitief Energielabel, versie 1.2, 16 september 2014

Method used for determining energy efficiency

RegistrationDate

20170814

The date when the energy label registered

Validity

20270814

The date until when the energy label is valid

PrimaryEnergyDemand

255

primary fossile energy demand expressed in kWh/m² per year (BENG2)

PercentageRenewable

17,2

% of energy coming from renewable sources

HeatDemand

181

heat demand expressed in kWh/m² per year

EnergyDemand

182

primary energy demand expressed in kWh/m² per year

Climate data features

The current climate is based on the period 1981-2010. It is mentioned as "currently" in the feature explanation.

Credits (Attribution) for the climate data

Esri Netherlands, Climate Impact Atlas, KNMI

Feature	Example	Explanation
subsidence_2020_2050_high	0.0283684033612987	The land subsidence, based on significant climate change, up to the period 2050.
subsidence_2020_2050_low	0.0266615749903464	The land subsidence, based on limited climate change, up to the period 2050.
subsidence_2020_2100_high	0.0559195945068944	The land subsidence, based on significant climate change, up to the period 2100.
subsidence_2020_2100_low	0.0508072813573541	The land subsidence, based on limited climate change, up to the period 2100.
soil_subsidence_due_elevation_2020_2050	0.2649501278801023	The soil subsidence due to elevation, up to the period 2050.
average_highest_groundwater_level_2050_high	0.0662050768733024	The average highest groundwater level, based on significant climate change, up to the period 2050. High groundwater levels can cause wet damage in agriculture and some nature types.
average_highest_groundwater_level_current	0.7322854995727539	The average highest groundwater level currently. High groundwater levels can cause wet damage in agriculture and some nature types.
average_lowest_groundwater_level_2050_high	-0.0944000035524368	The average lowest groundwater level, based on significant climate change, up to the period 2050. If the groundwater level is too low, damage can occur, for example to crops.
average_lowest_groundwater_level_2050_low	-0.0400299988687038	The average lowest groundwater level, based on limited climate change, up to the period 2050. If the groundwater level is too low, damage can occur, for example to crops.
average_lowest_groundwater_level_current	1.374940037727356	The average lowest groundwater level currently. If the groundwater level is too low, damage can occur, for example to crops.
sensitivity_to_water_erosion	99999.0	The sensitivity to water erosion. Land with slopes and relief is prone to erosion, especially if it is bare. Vegetation provides protection.
heat_map_perceived_temperature_2050_high		The perceived temperature on a hot summer day, based on limited climate change, up to the period 2050. The perceived temperature indicates how warm a person feels in a certain weather situation.
heat_map_perceived_temperature_current		The perceived temperature on a hot summer day currently. The perceived temperature indicates how warm a person feels in a certain weather situation.
heat_stress_due_to_warm_nights_2050_high	0.7507284879684448	The average number of tropical nights per year, based on limited climate change, up to the period 2050. Heat stress occurs when the body cannot get rid of excess heat. During a tropical night the temperature does not drop below 20 °C. The minimum temperature is therefore 20 °C or higher. Warm nights are an important factor in heat stress.
heat_stress_due_to_warm_nights_current	0.7507284879684448	The average number of tropical nights per year currently. Heat stress occurs when the body cannot get rid of excess heat. During a tropical night, the temperature does not drop below 20 °C. The minimum temperature is therefore 20 °C or higher. Warm nights are an important factor in heat stress.
seepage_and_infiltration_2050_high	0.102735698223114	The rate of erosion in mm per day, based on significant climate change, up to the period 2050. Leaving groundwater is called seepage and infiltration is the penetration of water into the ground. Human intervention can change the 'flux' between seepage and infiltration.
seepage_and_infiltration_current	0.1016992032527923	The rate of erosion in mm per day currently. Leaving groundwater is called seepage and infiltration is the penetration of water into the ground. Human intervention can change the 'flux' between seepage and infiltration.
lowest_groundwater_level_extremely_dry_summer_2050_high	-0.046509999781847	The expected development of the groundwater level in an extremely dry summer, based on significant climate change, up to the period 2050.
lowest_groundwater_level_extremely_dry_summer_2050_low	-0.0190699994564056	The expected development of the groundwater level in an extremely dry summer, based on limited climate change, up to the period 2050. Strong drop (>1m): -1 Strong drop (0.25-1m): (-1, -0,25) Some drop (0.1-0.25m): (-0.25, -1) No clear development: (-0.1, 0.1) Some rise (0.1-0.25m): (0.1, 0.25) Some rise (0.25 - 1m): (0.25, 1) Strong rise (>1 meter): (1, 6.220294952)
lowest_groundwater_level_extremely_dry_summer_current	1.496945023536682	The expected development of the groundwater level in an extremely dry summer currently, in meters below ground
wild_fire_sensitivity_2050_high		The chance of a wildfire, based on significant climate change, up to the period 2050.
wild_fire_sensitivity_current		The chance of a wildfire, currently.
flood_depth_extreme_probability	0.3700000047683716	The maximum flood depth based on extreme probability. Extreme probability: the probability that an area will be flooded approx. once every 10 years;
flood_depth_big_probability		The maximum flood depth based on high probability. High probability: the probability that an area will be flooded approx. once every 100 years;
flood_depth_small_probability	0.0718051269650459	The maximum flood depth based on small probability. Small probability: the probability that an area will be flooded approx. once every 100,000 years;
flood_depth_medium_probability		The maximum flood depth based on medium probability. Medium probability: the probability that an area will be flooded approx. once every 100,000 years;
location_based_flood_probability_2050_0cm	1.0	The total probability of flooding from the primary and regional water systems combined, per neighborhood, for 2050, with a minimum water depth of 0 cm. The chance that 1 person at 1 location per year has to deal with a flood is called the location-based flood risk.
location_based_flood_probability_2050_200cm		The total probability of flooding from the primary and regional water systems combined, per neighbourhood, for 2050, with a minimum water depth of 200 cm. The chance that 1 person at 1 location per year has to deal with a flood is called the location-based flood risk.
location_based_flood_probability_2050_20cm	1.0	The total probability of flooding from the primary and regional water systems combined, per neighbourhood, for 2050, with a minimum water depth of 20 cm. The chance that 1 person at 1 location per year has to deal with a flood is called the location-based flood risk.
location_based_flood_probability_2050_50cm		The total probability of flooding from the primary and regional water systems combined, per neighbourhood, for 2050, with a minimum water depth of 50 cm. The chance that 1 person at 1 location per year has to deal with a flood is called the location-based flood risk.
risk_of_drought_stress_2050_high		The risk of drought stress, based on significant climate change, up to the period 2050. Drought stress occurs when the soil dehydrates to a point that inhibits plant evaporation. Drought stress has consequences for agriculture and nature.
risk_of_drought_stress_current		The risk of drought stress, currently. Drought stress occurs when the soil dehydrates to a point that inhibits plant evaporation. Drought stress has consequences for agriculture and nature.
risk_of_subsoil_compaction_2050_high	901.0	The risk of subsoil compaction based on significant climate change, up to the period 2050. Subsoil compaction reduces the infiltration capacity, permeability, and moisture storage capacity of the soil.
risk_of_oxygen_otress_2050_high		The risk of oxygen stress, based on significant climate change, up to the period 2050. The more the soil is saturated with water, the more the supply of oxygen to plant roots is hindered. Heavy rainfall can therefore cause oxygen stress, which becomes more serious as the heat increases, because plants then need extra oxygen.
risk_of_oxygen_otress_current		The risk of oxygen stress currently. The more the soil is saturated with water, the more the supply of oxygen to plant roots is hindered. Heavy rainfall can therefore cause oxygen stress, which becomes more serious as the heat increases, because plants then need extra oxygen.
subsidence_okt16_okt18	1.0	The average soil subsidence over a period of 2 years (Oct 2016 – Oct 2018).
urban_heat_island_effect	0.6880000233650208	The average temperature difference, in degrees Celsius (°C), between the city and the countryside.
urban_infiltration_probabilities	18.0	The infiltration opportunities. It is based on a combination of the location’s scores in terms of infiltration capacity, storage capacity, and surface level slope
water_depth_intense_precipitation_1_per_1000_years		The maximum water depth that can occur in a location as a result of short-term intense precipitation. A shower of 140 mm in 2 hours was used for the modeling. Under the current climate, this shower occurs approximately once every 1000 years.
water_depth_intense_precipitation_1_per_100_years		The maximum water depth that can occur in a location as a result of short-term intense precipitation. A shower of 70 mm in 2 hours was used for the modeling. Under the current climate, this shower occurs approximately once every 100 years.
number_of_ice_days_2050_high	0-2	The average number of ice days per year, over a period of 30 years, based on significant climate change. On an ice day the maximum temperature is 0 °C or lower.
number_of_ice_days_2050_low	2-4	The average number of ice days per year, over a period of 30 years, based on limited climate change. On an ice day the maximum temperature is 0 °C or lower.
number_of_ice_days_current	8-10	The average number of ice days per year currently. On an ice day the maximum temperature is 0 °C or lower.
number_of_tropical_days_2050_low	3-6	The average number of tropical days per year, over a period of 30 years, based on limited climate change. On a tropical day the maximum temperature is 30 °C or higher.
number_of_tropical_days_current	0-3	The average number of tropical days per year, currently. On a tropical day the maximum temperature is 30 °C or higher.
number_of_frost_days_2050_high	10-20	The average number of frosty days per year, over a period of 30 years, based on significant climate change. On a frosty day the minimum temperature is 0 °C or lower.
number_of_frost_days_2050_low	30-40	The average number of frosty days per year, over a period of 30 years, based on limited climate change. On a frosty day the minimum temperature is 0 °C or lower.
number_of_frost_days_current	50-60	The average number of frosty days per year, currently. On a frosty day the minimum temperature is 0 °C or lower.
number_of_warm_days_2050_high	105-120	The average number of warm days per year, over a period of 30 years, based on significant climate change. On a warm day the maximum temperature is 20 °C or higher.
number_of_warm_days_2050_low	75-90	The average number of warm days per year, over a period of 30 years, based on limited climate change. On a warm day the maximum temperature is 20 °C or higher.
number_of_warm_days_current	60-75	The average number of warm days per year, currently. On a warm day the maximum temperature is 20 °C or higher.
number_of_summer_days_2050_high	30-40	The average number of summer days per year, over a period of 30 years, based on significant climate change. On a summer day the maximum temperature is 25 °C or higher.
number_of_summer_days_2050_low	20-30	The average number of summer days per year, over a period of 30 years, based on limited climate change. On a summer day the maximum temperature is 25 °C or higher.
number_of_summer_days_current	10-20	The average number of summer days per year, currently. On a summer day the maximum temperature is 25 °C or higher.
distance_to_coolness	0 - 200 meter	The distance between the house and the closes cool place. During heat waves and hot summer days it is important that you can cool down. That is why it is important that there are cool places nearby where you can quickly go in the heat.
natural_system_main_class	3 Laagveen	The landscape class of the location. The Netherlands is divided into 11 landscapes.
natural_system_sub_classa	Lv1 Laagveenvlakte	The landscape subclass of the location. The Netherlands is divided into 50 landscape sub-types. These subtypes differ from each other because different processes have contributed to their formation.
days_with_gte_15mm_2050_high	15-17	The average number of days per year that 15 mm or more precipitation falls, over a period of 30 years, based on significant climate change.
days_with_gte_15mm_2050_low	15-17	The average number of days per year that 15 mm or more precipitation falls, over a period of 30 years, based on limited climate change.
days_with_gte_15mm_current	13-15	The average number of days per year that 15 mm or more precipitation falls, currently.
days_with_gte_25mm_2050_high	4-5	The average number of days per year that 25 mm or more precipitation falls, over a period of 30 years, based on significant climate change.
days_with_gte_215mm_2050_low	3-4	The average number of days per year that 215 mm or more precipitation falls, over a period of 30 years, based on limited climate change.
days_with_gte_25mm_current	2-3	The average number of days per year that 25 mm or more precipitation falls, currently.
drought_sensitivity_groundwater_dependent_nature		The sensitivity to drought of this area if changes occur in groundwater.
annual_precipitation_2050_high	950-1000	The average annual precipitation in millimeters over a period of 30 years, based on significant climate change.
annual_precipitation_current	900-950	The average annual precipitation in millimeters currently.
annual_reference_evaporation_2050_high	610-630	The reference evaporation in millimeters per year, averaged over a period of 30 years, based on significant climate change. Radiation and temperature largely determine the amount of evaporation.
annual_reference_evaporation_current	570-590	The reference evaporation in millimeters per year, currently. Radiation and temperature largely determine the amount of evaporation.
probability_map_consequence_limitation	beperken schade bij ondiepe overstroming (20-50cm)	The chance of limiting the consequences of a flood.
agricultural_area		The agricultural. Possible values: grassland or arable farming. Agricultural land can be damaged by both drought and flooding. Drought and flooding can cause economic damage, especially in arable farming and floriculture.
longest_series_of_consecutive_summer_days_gte_25_days_2050_high	9-11	The longest series of consecutive summer days, over a period of 30 years, based on significant climate change. On a summer day the maximum temperature is 25 °C or higher.
longest_series_of_consecutive_summer_days_gte_25_days_current	5-7	The longest series of consecutive summer days, currently. On a summer day the maximum temperature is 25 °C or higher.
precipitation_winter_quarter_2050_high	250-275	The average winter precipitation in millimeters per year over a period of 30 years, up to 2050.
precipitation_winter_quarter_current	225-250	The average winter precipitation in millimeters per year currently.
precipitation_summer_quarter_2050_high	200-225	The average summer precipitation in millimeters per year over a period of 30 years, based on significant climate change. The summer precipitation has been calculated for the period June, July, and August.
precipitation_summer_quarter_current	225-250	The average summer precipitation in millimeters per year over a period of 30 years, currently. The current climate is based on the period 1981-2010.
development_probbility_groundwater_nuisance_2050_high	Aanmerkelijke toename kans	The risk of nuisance increase due to rising groundwater, over a period of 30 years, up to 2050, based on significant climate change. Groundwater flooding occurs when user functions are negatively affected by high groundwater levels.
potential_maximum_precipitation_deficit_once_per_10_years_2050_high	270 - 300	The potential maximum precipitation deficit, for a situation that occurs on average once every ten years, over a period of 30 years, up to 2050, based on significant climate change. The precipitation deficit is a measure of the drought and results from the difference between evaporation and precipitation during the period April to September.
potential_maximum_precipitation_deficit_once_per_10_years_current	210-240	The potential maximum precipitation deficit, for a situation that occurs on average once every ten years, currently. The precipitation deficit is a measure of the drought and results from the difference between evaporation and precipitation during the period April to September.
potential_maximum_precipitation_deficit_average_2050_high	210-240	The potential rainfall deficit for this area, over a period of 30 years, up to 2050, based on significant climate change. The potential precipitation deficit is a measure of the drought and results from the difference between evaporation and precipitation during the period April to September. The potential maximum rainfall deficit usually occurs at the end of summer. An increase in the precipitation deficit usually leads to a decrease in water availability in ground and surface water and an increase in water demand for water level management and irrigation.
potential_maximum_precipitation_deficit_average_current	150-180	The potential rainfall deficit for this area, currently. The potential precipitation deficit is a measure of the drought and results from the difference between evaporation and precipitation during the period April to September. The potential maximum rainfall deficit usually occurs at the end of summer. An increase in the precipitation deficit usually leads to a decrease in water availability in ground and surface water and an increase in water demand for water level management and irrigation.
risk_of_surface_water_warming_2050_high		The expected longest range of days of surface water with a minimum temperature of 20°C at this location in 2050, based on significant climate change.
risk_of_surface_water_warming_current		The expected longest range of days of surface water with a minimum temperature of 20°C at this location, currently.
surface_water_shortage_extremely_dry_year_2050_high	te weinig	The cause of the shortage of surface water, in an extremely dry year, in 2050, based on significant climate change.
surface_water_shortage_extremely_dry_year_current	geen problemen	The cause of the shortage of surface water, in an extremely dry year, currently.
surface_water_shortage_average_year_2050_high	geen problemen	The cause of the surface water shortage, in an averagely dry year, in 2050, based on significant climate change.
surface_water_shortage_average_year_current	geen problemen	The cause of the surface water shortage, in an averagely dry year, currently.
complete_map_of_climate_buffers		The opportunities for natural climate buffers.
neighborhood_typology	Tuinstad hoogbouw	The most common typology of the neighbourhood. The neighbourhood typologies have been determined for every urban area in the Netherlands, at postal code 6 level (e.g., 1234AB).

Feature

Example

Explanation

Value Interpretation & Ranges

subsidence_2020_2050_high

0.0283684033612987

The land subsidence, based on significant climate change, up to the period 2050.

subsidence_2020_2050_low

0.0266615749903464

The land subsidence, based on limited climate change, up to the period 2050.

subsidence_2020_2100_high

0.0559195945068944

The land subsidence, based on significant climate change, up to the period 2100.

subsidence_2020_2100_low

0.0508072813573541

The land subsidence, based on limited climate change, up to the period 2100.

soil_subsidence_due_elevation_2020_2050

0.2649501278801023

The soil subsidence due to elevation, up to the period 2050.

average_highest_groundwater_level_2050_high

0.0662050768733024

The average highest groundwater level, based on significant climate change, up to the period 2050. High groundwater levels can cause wet damage in agriculture and some nature types.

average_highest_groundwater_level_current

0.7322854995727539

The average highest groundwater level currently. High groundwater levels can cause wet damage in agriculture and some nature types.

average_lowest_groundwater_level_2050_high

-0.0944000035524368

The average lowest groundwater level, based on significant climate change, up to the period 2050. If the groundwater level is too low, damage can occur, for example to crops.

average_lowest_groundwater_level_2050_low

-0.0400299988687038

The average lowest groundwater level, based on limited climate change, up to the period 2050. If the groundwater level is too low, damage can occur, for example to crops.

average_lowest_groundwater_level_current

1.374940037727356

The average lowest groundwater level currently. If the groundwater level is too low, damage can occur, for example to crops.

sensitivity_to_water_erosion

99999.0

The sensitivity to water erosion. Land with slopes and relief is prone to erosion, especially if it is bare. Vegetation provides protection.

heat_map_perceived_temperature_2050_high

The perceived temperature on a hot summer day, based on limited climate change, up to the period 2050. The perceived temperature indicates how warm a person feels in a certain weather situation.

heat_map_perceived_temperature_current

The perceived temperature on a hot summer day currently. The perceived temperature indicates how warm a person feels in a certain weather situation.

heat_stress_due_to_warm_nights_2050_high

0.7507284879684448

The average number of tropical nights per year, based on limited climate change, up to the period 2050. Heat stress occurs when the body cannot get rid of excess heat. During a tropical night the temperature does not drop below 20 °C. The minimum temperature is therefore 20 °C or higher. Warm nights are an important factor in heat stress.

heat_stress_due_to_warm_nights_current

0.7507284879684448

The average number of tropical nights per year currently. Heat stress occurs when the body cannot get rid of excess heat. During a tropical night, the temperature does not drop below 20 °C. The minimum temperature is therefore 20 °C or higher. Warm nights are an important factor in heat stress.

seepage_and_infiltration_2050_high

0.102735698223114

The rate of erosion in mm per day, based on significant climate change, up to the period 2050. Leaving groundwater is called seepage and infiltration is the penetration of water into the ground. Human intervention can change the 'flux' between seepage and infiltration.

seepage_and_infiltration_current

0.1016992032527923

The rate of erosion in mm per day currently. Leaving groundwater is called seepage and infiltration is the penetration of water into the ground. Human intervention can change the 'flux' between seepage and infiltration.

lowest_groundwater_level_extremely_dry_summer_2050_high

-0.046509999781847

The expected development of the groundwater level in an extremely dry summer, based on significant climate change, up to the period 2050.

lowest_groundwater_level_extremely_dry_summer_2050_low

-0.0190699994564056

The expected development of the groundwater level in an extremely dry summer, based on limited climate change, up to the period 2050. Strong drop (>1m): -1

Strong drop (0.25-1m): (-1, -0,25)

Some drop (0.1-0.25m): (-0.25, -1)

No clear development: (-0.1, 0.1)

Some rise (0.1-0.25m): (0.1, 0.25)

Some rise (0.25 - 1m): (0.25, 1)

Strong rise (>1 meter): (1, 6.220294952)

lowest_groundwater_level_extremely_dry_summer_current

1.496945023536682

The expected development of the groundwater level in an extremely dry summer currently, in meters below ground

wild_fire_sensitivity_2050_high

The chance of a wildfire, based on significant climate change, up to the period 2050.

wild_fire_sensitivity_current

The chance of a wildfire, currently.

flood_depth_extreme_probability

0.3700000047683716

The maximum flood depth based on extreme probability.

Extreme probability: the probability that an area will be flooded approx. once every 10 years;

flood_depth_big_probability

The maximum flood depth based on high probability.

High probability: the probability that an area will be flooded approx. once every 100 years;

flood_depth_small_probability

0.0718051269650459

The maximum flood depth based on small probability.

Small probability: the probability that an area will be flooded approx. once every 100,000 years;

flood_depth_medium_probability

The maximum flood depth based on medium probability.

Medium probability: the probability that an area will be flooded approx. once every 100,000 years;

location_based_flood_probability_2050_0cm

1.0

The total probability of flooding from the primary and regional water systems combined, per neighborhood, for 2050, with a minimum water depth of 0 cm. The chance that 1 person at 1 location per year has to deal with a flood is called the location-based flood risk.

location_based_flood_probability_2050_200cm

The total probability of flooding from the primary and regional water systems combined, per neighbourhood, for 2050, with a minimum water depth of 200 cm. The chance that 1 person at 1 location per year has to deal with a flood is called the location-based flood risk.

location_based_flood_probability_2050_20cm

1.0

The total probability of flooding from the primary and regional water systems combined, per neighbourhood, for 2050, with a minimum water depth of 20 cm. The chance that 1 person at 1 location per year has to deal with a flood is called the location-based flood risk.

location_based_flood_probability_2050_50cm

The total probability of flooding from the primary and regional water systems combined, per neighbourhood, for 2050, with a minimum water depth of 50 cm. The chance that 1 person at 1 location per year has to deal with a flood is called the location-based flood risk.

risk_of_drought_stress_2050_high

The risk of drought stress, based on significant climate change, up to the period 2050. Drought stress occurs when the soil dehydrates to a point that inhibits plant evaporation. Drought stress has consequences for agriculture and nature.

risk_of_drought_stress_current

The risk of drought stress, currently. Drought stress occurs when the soil dehydrates to a point that inhibits plant evaporation. Drought stress has consequences for agriculture and nature.

risk_of_subsoil_compaction_2050_high

901.0

The risk of subsoil compaction based on significant climate change, up to the period 2050. Subsoil compaction reduces the infiltration capacity, permeability, and moisture storage capacity of the soil.

risk_of_oxygen_otress_2050_high

The risk of oxygen stress, based on significant climate change, up to the period 2050. The more the soil is saturated with water, the more the supply of oxygen to plant roots is hindered. Heavy rainfall can therefore cause oxygen stress, which becomes more serious as the heat increases, because plants then need extra oxygen.

risk_of_oxygen_otress_current

The risk of oxygen stress currently. The more the soil is saturated with water, the more the supply of oxygen to plant roots is hindered. Heavy rainfall can therefore cause oxygen stress, which becomes more serious as the heat increases, because plants then need extra oxygen.

subsidence_okt16_okt18

1.0

The average soil subsidence over a period of 2 years (Oct 2016 – Oct 2018).

urban_heat_island_effect

0.6880000233650208

The average temperature difference, in degrees Celsius (°C), between the city and the countryside.

urban_infiltration_probabilities

18.0

The infiltration opportunities. It is based on a combination of the location’s scores in terms of infiltration capacity, storage capacity, and surface level slope

water_depth_intense_precipitation_1_per_1000_years

The maximum water depth that can occur in a location as a result of short-term intense precipitation. A shower of 140 mm in 2 hours was used for the modeling. Under the current climate, this shower occurs approximately once every 1000 years.

water_depth_intense_precipitation_1_per_100_years

The maximum water depth that can occur in a location as a result of short-term intense precipitation. A shower of 70 mm in 2 hours was used for the modeling. Under the current climate, this shower occurs approximately once every 100 years.

number_of_ice_days_2050_high

0-2

The average number of ice days per year, over a period of 30 years, based on significant climate change. On an ice day the maximum temperature is 0 °C or lower.

number_of_ice_days_2050_low

2-4

The average number of ice days per year, over a period of 30 years, based on limited climate change. On an ice day the maximum temperature is 0 °C or lower.

number_of_ice_days_current

8-10

The average number of ice days per year currently. On an ice day the maximum temperature is 0 °C or lower.

number_of_tropical_days_2050_low

3-6

The average number of tropical days per year, over a period of 30 years, based on limited climate change. On a tropical day the maximum temperature is 30 °C or higher.

number_of_tropical_days_current

0-3

The average number of tropical days per year, currently. On a tropical day the maximum temperature is 30 °C or higher.

number_of_frost_days_2050_high

10-20

The average number of frosty days per year, over a period of 30 years, based on significant climate change. On a frosty day the minimum temperature is 0 °C or lower.

number_of_frost_days_2050_low

30-40

The average number of frosty days per year, over a period of 30 years, based on limited climate change. On a frosty day the minimum temperature is 0 °C or lower.

number_of_frost_days_current

50-60

The average number of frosty days per year, currently. On a frosty day the minimum temperature is 0 °C or lower.

number_of_warm_days_2050_high

105-120

The average number of warm days per year, over a period of 30 years, based on significant climate change. On a warm day the maximum temperature is 20 °C or higher.

number_of_warm_days_2050_low

75-90

The average number of warm days per year, over a period of 30 years, based on limited climate change. On a warm day the maximum temperature is 20 °C or higher.

number_of_warm_days_current

60-75

The average number of warm days per year, currently. On a warm day the maximum temperature is 20 °C or higher.

number_of_summer_days_2050_high

30-40

The average number of summer days per year, over a period of 30 years, based on significant climate change. On a summer day the maximum temperature is 25 °C or higher.

number_of_summer_days_2050_low

20-30

The average number of summer days per year, over a period of 30 years, based on limited climate change. On a summer day the maximum temperature is 25 °C or higher.

number_of_summer_days_current

10-20

The average number of summer days per year, currently. On a summer day the maximum temperature is 25 °C or higher.

distance_to_coolness

0 - 200 meter

The distance between the house and the closes cool place. During heat waves and hot summer days it is important that you can cool down. That is why it is important that there are cool places nearby where you can quickly go in the heat.

natural_system_main_class

3 Laagveen

The landscape class of the location. The Netherlands is divided into 11 landscapes.

natural_system_sub_classa

Lv1 Laagveenvlakte

The landscape subclass of the location. The Netherlands is divided into 50 landscape sub-types. These subtypes differ from each other because different processes have contributed to their formation.

days_with_gte_15mm_2050_high

15-17

The average number of days per year that 15 mm or more precipitation falls, over a period of 30 years, based on significant climate change.

days_with_gte_15mm_2050_low

15-17

The average number of days per year that 15 mm or more precipitation falls, over a period of 30 years, based on limited climate change.

days_with_gte_15mm_current

13-15

The average number of days per year that 15 mm or more precipitation falls, currently.

days_with_gte_25mm_2050_high

4-5

The average number of days per year that 25 mm or more precipitation falls, over a period of 30 years, based on significant climate change.

days_with_gte_215mm_2050_low

3-4

The average number of days per year that 215 mm or more precipitation falls, over a period of 30 years, based on limited climate change.

days_with_gte_25mm_current

2-3

The average number of days per year that 25 mm or more precipitation falls, currently.

drought_sensitivity_groundwater_dependent_nature

The sensitivity to drought of this area if changes occur in groundwater.

annual_precipitation_2050_high

950-1000

The average annual precipitation in millimeters over a period of 30 years, based on significant climate change.

annual_precipitation_current

900-950

The average annual precipitation in millimeters currently.

annual_reference_evaporation_2050_high

610-630

The reference evaporation in millimeters per year, averaged over a period of 30 years, based on significant climate change. Radiation and temperature largely determine the amount of evaporation.

annual_reference_evaporation_current

570-590

The reference evaporation in millimeters per year, currently. Radiation and temperature largely determine the amount of evaporation.

probability_map_consequence_limitation

beperken schade bij ondiepe overstroming (20-50cm)

The chance of limiting the consequences of a flood.

agricultural_area

The agricultural. Possible values: grassland or arable farming. Agricultural land can be damaged by both drought and flooding. Drought and flooding can cause economic damage, especially in arable farming and floriculture.

longest_series_of_consecutive_summer_days_gte_25_days_2050_high

9-11

The longest series of consecutive summer days, over a period of 30 years, based on significant climate change. On a summer day the maximum temperature is 25 °C or higher.

longest_series_of_consecutive_summer_days_gte_25_days_current

5-7

The longest series of consecutive summer days, currently. On a summer day the maximum temperature is 25 °C or higher.

precipitation_winter_quarter_2050_high

250-275

The average winter precipitation in millimeters per year over a period of 30 years, up to 2050.

precipitation_winter_quarter_current

225-250

The average winter precipitation in millimeters per year currently.

precipitation_summer_quarter_2050_high

200-225

The average summer precipitation in millimeters per year over a period of 30 years, based on significant climate change. The summer precipitation has been calculated for the period June, July, and August.

precipitation_summer_quarter_current

225-250

The average summer precipitation in millimeters per year over a period of 30 years, currently. The current climate is based on the period 1981-2010.

development_probbility_groundwater_nuisance_2050_high

Aanmerkelijke toename kans

The risk of nuisance increase due to rising groundwater, over a period of 30 years, up to 2050, based on significant climate change. Groundwater flooding occurs when user functions are negatively affected by high groundwater levels.

potential_maximum_precipitation_deficit_once_per_10_years_2050_high

270 - 300

The potential maximum precipitation deficit, for a situation that occurs on average once every ten years, over a period of 30 years, up to 2050, based on significant climate change. The precipitation deficit is a measure of the drought and results from the difference between evaporation and precipitation during the period April to September.

potential_maximum_precipitation_deficit_once_per_10_years_current

210-240

The potential maximum precipitation deficit, for a situation that occurs on average once every ten years, currently. The precipitation deficit is a measure of the drought and results from the difference between evaporation and precipitation during the period April to September.

potential_maximum_precipitation_deficit_average_2050_high

210-240

The potential rainfall deficit for this area, over a period of 30 years, up to 2050, based on significant climate change. The potential precipitation deficit is a measure of the drought and results from the difference between evaporation and precipitation during the period April to September. The potential maximum rainfall deficit usually occurs at the end of summer. An increase in the precipitation deficit usually leads to a decrease in water availability in ground and surface water and an increase in water demand for water level management and irrigation.

potential_maximum_precipitation_deficit_average_current

150-180

The potential rainfall deficit for this area, currently. The potential precipitation deficit is a measure of the drought and results from the difference between evaporation and precipitation during the period April to September. The potential maximum rainfall deficit usually occurs at the end of summer. An increase in the precipitation deficit usually leads to a decrease in water availability in ground and surface water and an increase in water demand for water level management and irrigation.

risk_of_surface_water_warming_2050_high

The expected longest range of days of surface water with a minimum temperature of 20°C at this location in 2050, based on significant climate change.

risk_of_surface_water_warming_current

The expected longest range of days of surface water with a minimum temperature of 20°C at this location, currently.

surface_water_shortage_extremely_dry_year_2050_high

te weinig

The cause of the shortage of surface water, in an extremely dry year, in 2050, based on significant climate change.

surface_water_shortage_extremely_dry_year_current

geen problemen

The cause of the shortage of surface water, in an extremely dry year, currently.

surface_water_shortage_average_year_2050_high

geen problemen

The cause of the surface water shortage, in an averagely dry year, in 2050, based on significant climate change.

surface_water_shortage_average_year_current

geen problemen

The cause of the surface water shortage, in an averagely dry year, currently.

complete_map_of_climate_buffers

The opportunities for natural climate buffers.

neighborhood_typology

Tuinstad hoogbouw

The most common typology of the neighbourhood. The neighbourhood typologies have been determined for every urban area in the Netherlands, at postal code 6 level (e.g., 1234AB).

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Last updated 27 days ago