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
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	Value Interpretation & Ranges
subsidence_2020_2050_high	0.0283684033612987	The land subsidence, based on significant climate change, up to the period 2050.	Value interpretation Min value Max value 'No prediction possible' -1.0 -1.0 'Negligible (<3cm)' -1.0 0.03 'Limited (3-10cm)' 0.03 0.1 'Moderate (10-20cm)' 0.1 0.2 'Quite strong (20-40cm)' 0.2 0.4 'Strong (40-60cm)' 0.4 0.6 'Very strong (40-60cm)' 0.6 2.0
subsidence_2020_2050_low	0.0266615749903464	The land subsidence, based on limited climate change, up to the period 2050.	Value interpretation Min value Max value 'No prediction possible' -1.0 -1.0 'Negligible (<3cm)' -1.0 0.03 'Limited (3-10cm)' 0.03 0.1 'Moderate (10-20cm)' 0.1 0.2 'Quite strong (20-40cm)' 0.2 0.4 'Strong (40-60cm)' 0.4 0.6 'Very strong (40-60cm)' 0.6 2.0
subsidence_2020_2100_high	0.0559195945068944	The land subsidence, based on significant climate change, up to the period 2100.	Value interpretation Min value Max value 'No prediction possible' -1.0 -1.0 'Negligible (<3cm)' -1.0 0.03 'Limited (3-10cm)' 0.03 0.1 'Moderate (10-20cm)' 0.1 0.2 'Quite strong (20-40cm)' 0.2 0.4 'Strong (40-60cm)' 0.4 0.6 'Very strong (40-60cm)' 0.6 2.0
subsidence_2020_2100_low	0.0508072813573541	The land subsidence, based on limited climate change, up to the period 2100.	Value interpretation Min value Max value 'No prediction possible' -1.0 -1.0 'Negligible (<3cm)' -1.0 0.03 'Limited (3-10cm)' 0.03 0.1 'Moderate (10-20cm)' 0.1 0.2 'Quite strong (20-40cm)' 0.2 0.4 'Strong (40-60cm)' 0.4 0.6 'Very strong (40-60cm)' 0.6 2.0
soil_subsidence_due_elevation_2020_2050	0.2649501278801023	The soil subsidence due to elevation, up to the period 2050.	Value interpretation Min value Max value 'Not worth mentioning' 0.03 0.03 '3 - 10 cm' 0.03 0.1 '10 - 25 cm' 0.1 0.25 '25 - 50 cm' 0.25 0.50 '50 - 100 cm' 0.50 1.00 '> 100 cm' 1.00 inf
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.	Value interpretation Min value Max value 'No prediction possible' -1.0 -1.0 'Negligible (<3cm)' -1.0 0.03 'Limited (3-10cm)' 0.03 0.1 'Moderate (10-20cm)' 0.1 0.2 'Quite strong (20-40cm)' 0.2 0.4 'Strong (40-60cm)' 0.4 0.6 'Very strong (40-60cm)' 0.6 2.0
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.	Value interpretation Min value Max value 'No prediction possible' -1.0 -1.0 'Negligible (<3cm)' -1.0 0.03 'Limited (3-10cm)' 0.03 0.1 'Moderate (10-20cm)' 0.1 0.2 'Quite strong (20-40cm)' 0.2 0.4 'Strong (40-60cm)' 0.4 0.6 'Very strong (40-60cm)' 0.6 2.0
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.	Value interpretation Min value Max value 'No prediction possible' -1.0 -1.0 'Negligible (<3cm)' -1.0 0.03 'Limited (3-10cm)' 0.03 0.1 'Moderate (10-20cm)' 0.1 0.2 'Quite strong (20-40cm)' 0.2 0.4 'Strong (40-60cm)' 0.4 0.6 'Very strong (40-60cm)' 0.6 2.0
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.	Value interpretation Min value Max value '<= 4.633e-6' 0.000005 0.000005 '<0.2' 0.000005 0.2 '0,2 - 0,4 m' 0.2 0.4 '0,4 - 0,6 m ' 0.4 0.6 '0,6 - 0,8 m' 0.6 0.8 '0,8 - 1 m ' 0.8 1.0 '1 - 1,5 m ' 1.0 1.5 '1,5 - 2 m' 1.5 2.0 '>2 m ' 2.0 inf
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.	Value interpretation Min value Max value '<= 4.633e-6' 0.000005 0.000005 '<0.2' 0.000005 0.2 '0,2 - 0,4 m' 0.2 0.4 '0,4 - 0,6 m ' 0.4 0.6 '0,6 - 0,8 m' 0.6 0.8 '0,8 - 1 m ' 0.8 1.0 '1 - 1,5 m ' 1.0 1.5 '1,5 - 2 m' 1.5 2.0 '>2 m ' 2.0 inf
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.	Value interpretation Min value Max value 26°C of lager 23.0 23.0 27°C 23.0 27.0 28°C 27.0 28.0 … … … 52°C 51.0 52.0 53°C 52.0 53.0
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.	Value interpretation Min value Max value 26°C of lager 23.0 23.0 27°C 23.0 27.0 28°C 27.0 28.0 … … … 48°C 47.0 48.0 49°C 48.0 49.0
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.	Value interpretation Min value Max value 1 day 0.2894 0.2894 - 0.2894 0.2899 - 0.2899 0.3 1 week 0.3 0.45 - 0.45 0.55 2 weeks 0.55 0.65 - 0.65 0.75 3 weeks 0.75 0.85 - 0.85 0.95 >1 month 0.95 2.8516
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.	Value Interpretation Min value Max value 1 day 0.2894 0.2894 - 0.2894 0.45 - 0.45 0.6 1 week 0.6 0.75 - 0.75 0.9 2 weeks 0.9 1.0 - 1.0 2.82 3 weeks 2.82 2.83 - 2.83 2.84 >1 month 2.84 2.8516
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.	Value interpretation Min value Max value Clear increase in shedding (>1mm/day) -1.0 -1.0 (0.5-1mm/day) -1.0 -0.5 Some increase in shedding (0.1-0.5mm/day) -0.5 -0.1 No clear development -0.1 0.1 Some increase in seepage (0.1-0.5mm/day) 0.1 0.5 (0.5-1mm/day) 0.5 1.0 Clear increase in seepage (>1mm/day) 1.0 inf
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.	Value interpretation Min value Max value Strong seepage (>2 mm/day) -2.0 -2.0 (1-2 mm/day) -2.0 -1.0 (0.5-1 mm/day) -1.0 -0.5 Some seepage (0.1-0.5 mm/day) -0.5 -0.1 Little or no flux -0.1 0.1 Some change (0.1-0.5 mm/day) 0.1 0.5 (0.5-1 mm/day) 0.5 1.0
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.	Value interpretation Min value Max value Strong drop (>1m) -1.0 -1.0 (0.25-1m) -1.0 -0.25 Some drop (0.1-0.25m) -0.25 -0.1 No clear development -0.1 0.1 Some rise (0.1-0.25m) 0.1 0.25 (0.25 - 1m) 0.25 1.0 Strong rise (>1 meter) 1.0 6.220294952
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)	Value interpretation Min value Max value Strong drop (>1m) -1.0 -1.0 (0.25-1m) -1.0 -0.25 Some drop (0.1-0.25m) -0.25 -0.1 No clear development -0.1 0.1 Some rise (0.1-0.25m) 0.1 0.25 (0.25 - 1m) 0.25 1.0 Strong rise (>1 meter) 1.0 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	Value interpretation Min value Max value < 0,2 0.2 0.2 0,2 - 0,4 0.2 0.4 0,4 - 0,6 0.4 0.6 0,6 - 0,8 meters below ground level 0.6 0.8 0,8 - 1 0.8 1.0 1- 1,5 1.0 1.5 1,5 - 2 1.5 2.0 > 2 2.0 251.1925964
wild_fire_sensitivity_2050_high		The chance of a wildfire, based on significant climate change, up to the period 2050.	Value interpretation Value Low 1.0 Medium 2.0 High 3.0
wild_fire_sensitivity_current		The chance of a wildfire, currently.	Value interpretation Value Low 1.0 Medium 2.0 High 3.0
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;	Depth min value max value < 0.5 meter 0.0 0.5 0.5 - 1.0 meter 0.5 1.0 1.0 - 1.5 meter 1.0 1.5 1.5 - 2.0 meter 1.5 2.0 2.0 - 5.0 meter 2.0 5.0 > 5.0 meter 5.0 inf
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;	Depth min value max value < 0.5 meter 0.0 0.5 0.5 - 1.0 meter 0.5 1.0 1.0 - 1.5 meter 1.0 1.5 1.5 - 2.0 meter 1.5 2.0 2.0 - 5.0 meter 2.0 5.0 > 5.0 meter 5.0 inf
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;	Depth min value max value < 0.5 meter 0.0 0.5 0.5 - 1.0 meter 0.5 1.0 1.0 - 1.5 meter 1.0 1.5 1.5 - 2.0 meter 1.5 2.0 2.0 - 5.0 meter 2.0 5.0 > 5.0 meter 5.0 inf
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;	Depth min value max value < 0.5 meter 0.0 0.5 0.5 - 1.0 meter 0.5 1.0 1.0 - 1.5 meter 1.0 1.5 1.5 - 2.0 meter 1.5 2.0 2.0 - 5.0 meter 2.0 5.0 > 5.0 meter 5.0 inf
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.	Value interpretation value Extremely small chance: <1/30,000 per year 1.0 Very small chance: 1/3,000 to 1/30,000 per year 2.0 Small chance: 1/300 to 1/3,000 per year 3.0 Medium chance: 1/30 to 1/300 per year 4.0 High chance: > 1/30 per year 5.0
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.	Value interpretation value Extremely small chance: <1/30,000 per year 1.0 Very small chance: 1/3,000 to 1/30,000 per year 2.0 Small chance: 1/300 to 1/3,000 per year 3.0 Medium chance: 1/30 to 1/300 per year 4.0 High chance: > 1/30 per year 5.0
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.	Value interpretation value Extremely small chance: <1/30,000 per year 1.0 Very small chance: 1/3,000 to 1/30,000 per year 2.0 Small chance: 1/300 to 1/3,000 per year 3.0 Medium chance: 1/30 to 1/300 per year 4.0 High chance: > 1/30 per year 5.0
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.	Value interpretation value Extremely small chance: <1/30,000 per year 1.0 Very small chance: 1/3,000 to 1/30,000 per year 2.0 Small chance: 1/300 to 1/3,000 per year 3.0 Medium chance: 1/30 to 1/300 per year 4.0 High chance: > 1/30 per year 5.0
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 min value max value Low (annual yield loss <10% for grass) 0.988235294 20.0 Moderate (annual yield loss 10%-20% for grass) 20.0 30.0 High (annual yield loss >20% for grass) 30.0 42.0
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 min value max value Low (annual yield loss <10% for grass) 0.870588235 20.0 Moderate (annual yield loss 10%-20% for grass) 20.0 30.0 High (annual yield loss >20% for grass) 30.0 37.0
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 value Very limited 1.0 Limited 2.0 Moderate 3.0 Big 4.0 Very big 5.0 Limited by peat layers 10.0 Naturally dense 11.0
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 min value max value Low (<15% annual yield loss in grass) 10.0 10.0 Moderate (15%-40% annual yield loss in grass) 10.0 25.0 High (>40% annual yield loss in grass) 25.0 68.0
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.	Risk min value max value Low (<15% annual yield loss in grass) 10.0 10.0 Moderate (15%-40% annual yield loss in grass) 10.0 25.0 High (>40% annual yield loss in grass) 25.0 68.0
subsidence_okt16_okt18	1.0	The average soil subsidence over a period of 2 years (Oct 2016 – Oct 2018).	Value interpretation value Little drop from 1.0 Continuous significant decrease 2.0 Significant decrease (more than previous period) 3.0 Lots of decrease 4.0
urban_heat_island_effect	0.6880000233650208	The average temperature difference, in degrees Celsius (°C), between the city and the countryside.	Temperature range min value max value 0-0.2 °C 0.0 0.0 0.2-0.4 °C 0.0 0.2 0.4-0.6 °C 0.2 0.4 0.6-0.8 °C 0.4 0.6 0.8-1.0 °C 0.6 0.8 1.0-1.2 °C 0.8 1.0 1.2-1.4 °C 1.0 1.2 1.4-1.6 °C 1.2 1.4 1.6-1.8 °C 1.4 1.6 1.8-2.0 °C 1.6 1.8 >2 °C 1.8 inf
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.	Depth min value max value 5 - 10 cm 1.0 1.0 10 - 15 cm 1.0 2.0 15 - 20 cm 2.0 3.0 20 - 30 cm 3.0 4.0 > 30 cm 4.0 5.0
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.	Depth min value max value 5 - 10 cm 1.0 1.0 10 - 15 cm 1.0 2.0 15 - 20 cm 2.0 3.0 20 - 30 cm 3.0 4.0 > 30 cm 4.0 5.0
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.
natural_system_sub_class_copy	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.
agricultural_area_copy		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).