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TNO Flasksampler ICOS release H2 at 207m at Cabauw + (ICOS Final Fully Quality Controlled Observational Data (Level 2) for flask samples analysed on molar fraction of atmospheric H2 at 207m)
TNO Flasksampler ICOS release CO2 at 207m at Cabauw + (ICOS Final Fully Quality Controlled Observational Data (Level 2) for flask samples analysed on molar fraction of atmospheric CO2 at 207m)
TNO Flasksampler ICOS release dO2N2 207m at Cabauw + (ICOS Final Fully Quality Controlled Observational Data (Level 2) for flask samples analysed on molar fraction of atmospheric dO2N2 at 207m)
TNO Picarro5310 ICOS ATC Level 2 N2O at 027m at Cabauw + (ICOS Final Fully Quality Controlled Observational Data (Level 2) on molar fraction of atmospheric N2O at 027m)
TNO Flasksampler ICOS release d13C-CO2 207m at Cabauw + (ICOS Final Fully Quality Controlled Observational Data (Level 2) for flask samples analysed on molar fraction of atmospheric d13C-CO2 at 207m)
TNO Picarro2301 ICOS ATC Level 2 CO2 at 067m at Cabauw + (ICOS Final Fully Quality Controlled Observational Data (Level 2) on molar fraction of atmospheric CO2 at 067m)
TNO Flasksampler ICOS release 14C at 207m at Cabauw + (ICOS Final Fully Quality Controlled Observational Data (Level 2) for 14C in CO2 at 207m in two-weekly integrated samples with the ICOS rotating denuder sampler)
TU Delft optical disdrometer Thies-001 at Cabauw + (In-situ measurements of drop size distributions and rain rates at Lutjewad, with a temporal resolution of 1 minute, acquired by a Thies optical disdrometer.)
TU Delft optical disdrometer Parsivel² PAR007 in the meteorological tower at Cabauw + (In-situ measurements of raindrop size dist … In-situ measurements of raindrop size distributions, fall velocities, drop number concentrations and surface rain rates recorded by an OTT Parsivel2 disdrometer named "PAR007" at a height of 180 meters in the meteorological tower of Cabauw. This highly unusual location for a precipitation sensor was specifically chosen to study the effect of wind, turbulence and shielding on raindrop size distributions, as well as to quantify the vertical variability of rain near the surface. Two other disdrometers "PAR001_Cabauw" and "PAR002_Cabauw" located on the ground, approximately 200 meters away can be used as a reference to assess biases and measurement uncertainty. The site also features a vertically profiling micro-rain radar named "MRR002_Cabauw".ng micro-rain radar named "MRR002_Cabauw".)
TU Delft optical disdrometer Parsivel² PAR009 at Lutjewad + (In-situ measurements of raindrop size dist … In-situ measurements of raindrop size distributions, fall velocities, drop number concentrations and surface rain rates recorded by an OTT Parsivel2 disdrometer named "PAR009" at a height of 3 meters at the Lutjewad atmospheric measurement station on the northern coast of the Netherlands, approximately 30 km northeast from the city of Groningen. The rural landscape to the south consists mainly of pasture and cropland with patches of forested land with livestock dominated by dairy cows and sheep. Set up directly behind the Wadden Sea dike, the site features a 60 meter tall sampling tower, a 10 meter platform, a laboratory building, and an aerosol laboratory container. The station monitors greenhouse gases and trace gas species, sampling aerosol number, size, and composition at different altitudes. Lutjewad is part of the European research infrastructure ICOS, providing continuous greenhouse gas concentrations. The coastal location means that the site samples relatively clean marine background air in conditions of northerly winds and more polluted air masses during conditions of south-easterly and south-westerly winds.f south-easterly and south-westerly winds.)
TU Delft optical disdrometer Parsivel² PAR002 at Cabauw + (In-situ measurements of raindrop size dist … In-situ measurements of raindrop size distributions, fall velocities, drop number concentrations and surface rain rates recorded by an OTT Parsivel2 disdrometer named "PAR002" at the remote sensing site in Cabauw. Note that "PAR002" is co-located with another identical disdrometer called "PAR001". This co-location can be used to cross-check data, perform quality control and/or assess measurement uncertainty due to sensor calibration, random sampling effects and environmental effects such as wind speed/direction which are known to substantially affect the accuracy of optical disdrometers.fect the accuracy of optical disdrometers.)
TU Delft optical disdrometer Parsivel² PAR005 at De Zweth + (In-situ measurements of raindrop size dist … In-situ measurements of raindrop size distributions, fall velocities, drop number concentrations and surface rain rates recorded by an OTT Parsivel2 disdrometer named "PAR005" in De Zweth, The Netherlands. Situated approximately 7 km to the North West of Rotterdam, and 4 km South East of Delft campus, Zweth is a small town along the Schie river, at the intersection of the historical areas of Delfland and Schieland. The same site also features a micro-rain radar "MRR004_DeZweth" (since February 2022), replaced by "MRR006_DeZweth" (since August 2022) and a Davis weather station "Davis003_DeZweth" (since May 2023). All sensors are placed on top of an air quality monitoring container belonging to TNO, at a height of approx. 4 meters.g to TNO, at a height of approx. 4 meters.)
TU Delft optical disdrometer Parsivel² PAR003 (mobile) + (In-situ measurements of raindrop size dist … In-situ measurements of raindrop size distributions, fall velocities, drop number concentrations and surface rain rates recorded by an OTT Parsivel2 disdrometer named "PAR003" at the Green Village site in Delft. Note that the Green Village site is different from the other Ruisdael sites. Its primary purpose is to allow researchers to test sensors, perform calibration and develop new hardware/software solutions. The Green Village also serves as a temporary home basis for all the mobile sensors used during field campaigns. Due to the special nature of this site, data quality, reliability and availability may be lower than at other locations. There are also some nearby obstacles such as trees and fences which may affect the accuracy of the precipitation measurements depending on local wind patterns.urements depending on local wind patterns.)
TU Delft optical disdrometer Parsivel² PAR006 at Slufter + (In-situ measurements of raindrop size dist … In-situ measurements of raindrop size distributions, fall velocities, drop number concentrations and surface rain rates recorded by an OTT Parsivel2 disdrometer named "PAR006" in Slufter, The Netherlands. Located in the Maasvlakte Rotterdam, The Slufter is a large-scale storage site for contaminated sludge in the southwestern part of the Rotterdam Maasvlakte, approximately 31 km West of the city center of Rotterdam. Along the ring dike of the Slufter, several wind turbines belong to the Windpark Slufterdam are providing electricity for the region. The same site also features a micro-rain radar "MRR005_Slufter" (since March 2022). All sensors are placed on top of an air quality monitoring container belonging to TNO, at a height of approx. 4 meters. The rough climate conditions near the coast of the North Sea, with high winds, salt, and sand creates a very challenging environment for long-term weather observations. Consequently, data availability tends to be lower than at other sites, due to frequent maintenance and technical issues.frequent maintenance and technical issues.)
TU Delft optical disdrometer Parsivel² PAR004 at Westmaas + (In-situ measurements of raindrop size dist … In-situ measurements of raindrop size distributions, fall velocities, drop number concentrations and surface rain rates recorded by an OTT Parsivel2 disdrometer named "PAR004" in Westmaas, The Netherlands. Westmaas is a village in the Dutch province of South Holland located approximately 15 km south of the city centre of Rotterdam, south of the old Meuse. The same site also features a micro-rain radar "MRR003_Westmaas" (since June 2022) and a Davis weather station "Davis003_Westmaas" (since May 2023). All sensors are placed on top of an air quality monitoring container belonging to TNO, at a height of approx. 4 meters. The container is located approximately 1.5 km to the West of the village of Westmaas, in a predominantly flat and rural area.s, in a predominantly flat and rural area.)
TU Delft optical disdrometer Parsivel² PAR001 at Cabauw + (In-situ measurements of raindrop size dist … In-situ measurements of raindrop size distributions, fall velocities, drop number concentrations and surface rain rates recorded by an OTT Parsivel2 disdrometer named "PAR001" at the remote sensing site in Cabauw. Note that "PAR001" is co-located with another identical disdrometer called "PAR002". This co-location can be used to cross-check data, perform quality control and/or assess measurement uncertainty due to sensor calibration, random sampling effects and environmental effects such as wind speed/direction which are known to substantially affect the accuracy of optical disdrometers.fect the accuracy of optical disdrometers.)
TU Delft weather station davis-005 at Rijnhaven + (In-situ measurements of temperature, press … In-situ measurements of temperature, pressure, relative humidity, rain, solar irradiance and wind by a Davis Vantage Pro2 weather station named "Davis-005" at Rijnhaven.This station is part of the Rotterdam Atmospheric Measurement Network (RAMN), funded with the help of TU Delft strategic funds, in collaboration with the Ruisdael Observatory.llaboration with the Ruisdael Observatory.)
TU Delft weather station davis-002 at De Zweth + (In-situ measurements of temperature, press … In-situ measurements of temperature, pressure, relative humidity, rain, solar irradiance and wind (at a 1 minute temporal resolution) by a Davis Vantage Pro2 weather station named "Davis-002" at de Zweth in the Netherlands. Situated approximately 7 km to the North West of Rotterdam, and 4 km South East of Delft campus, Zweth is a small town along the Schie river, at the intersection of the historical areas of Delfland and Schieland. The same site also features a micro-rain radar "MRR004_DeZweth" (since February 2022), replaced by "MRR006_DeZweth" (since August 2022) and a Parsivel optical disdrometer "PAR005_DeZweth" (since February 2022). All sensors are placed on top of an air quality monitoring container belonging to TNO, at a height of approx. 4 meters.This station is part of The Rotterdam Atmospheric Measurement Network (RAMN) established with the help of TU Delft strategic funds, in collaboration with the Ruisdael Observatory at TU Delft.with the Ruisdael Observatory at TU Delft.)
TU Delft weather station davis-003 at Westmaas + (In-situ measurements of temperature, press … In-situ measurements of temperature, pressure, relative humidity, rain, solar irradiance and wind (at a temporal resolution of 1 minute) by a Davis Vantage Pro2 weather station named "Davis-003" at Westmaas, The Netherlands. Westmaas is a village in the Dutch province of South Holland located approximately 15 km south of the city centre of Rotterdam, south of the old Meuse. The same site also features a Parsivel optical disdrometer "PAR004_Westmaas" (since October 2021), and a vertically pointing micro-rain radar "MRR003_Westmaas" (since June 2022). All sensors are placed on top of an air quality monitoring container belonging to TNO, at a height of approx. 4 meters. The container is located approximately 1.5 km to the West of the village of Westmaas, in a predominantly flat and rural area.This station is part of the Rotterdam Atmospheric Measurement Network (RAMN), funded with the help of TU Delft strategic funds, in collaboration with the Ruisdael Observatory.llaboration with the Ruisdael Observatory.)
TU Delft weather station davis-007 at Handelsplein + (In-situ measurements of temperature, press … In-situ measurements of temperature, pressure, relative humidity, rain, solar irradiance and wind by a Davis Vantage Pro2 weather station named "Davis-007" at Handelsplein, Rotterdam, The Netherlands. The station is placed on a pole, at a height of 3 meters, with some small nearby trees. This station is part of the Rotterdam Atmospheric Measurement Network (RAMN), funded with the help of TU Delft strategic funds, in collaboration with the Ruisdael Observatory.llaboration with the Ruisdael Observatory.)
TU Delft weather station davis-006 at EUR campus + (In-situ measurements of temperature, press … In-situ measurements of temperature, pressure, relative humidity, rain, solar irradiance and wind by a Davis Vantage Pro2 weather station named "Davis-006" at Erasmus University Rotterdam (EUR campus). The station is located on the Sanders building roof, at a height of 29 meters.This station is part of the Rotterdam Atmospheric Measurement Network (RAMN), funded with the help of TU Delft strategic funds, in collaboration with the Ruisdael Observatory.llaboration with the Ruisdael Observatory.)
TU Delft weather station davis-008 at Platform Zero + (In-situ measurements of temperature, press … In-situ measurements of temperature, pressure, relative humidity, rain, solar irradiance and wind by a Davis Vantage Pro2 weather station named "Davis-008" at Platform zero, Rotterdam, The Netherlands. The station is placed on a flat roof, at Galileistraat 33, 3029 AM Rotterdam, at a height of approx. 10 meters. This station is part of the Rotterdam Atmospheric Measurement Network (RAMN), funded with the help of TU Delft strategic funds, in collaboration with the Ruisdael Observatory.llaboration with the Ruisdael Observatory.)
TU Delft weather station davis-009 at Hofbgenpark + (In-situ measurements of temperature, press … In-situ measurements of temperature, pressure, relative humidity, rain, solar irradiance and wind by a Davis Vantage Pro2 weather station named "Davis-009" at Hofbogenpark, Rotterdam, The Netherlands. The station is placed on a roof at Luchtsingel, Raampoortstraat 10, 3032 AH Rotterdam, at a height of approx. 8 metersThis station is part of the Rotterdam Atmospheric Measurement Network (RAMN), funded with the help of TU Delft strategic funds, in collaboration with the Ruisdael Observatory.llaboration with the Ruisdael Observatory.)
TU Delft weather station davis-004 at Schiedam DCMR + (In-situ measurements of temperature, press … In-situ measurements of temperature, pressure, relative humidity, rain, solar irradiance and wind by a Davis Vantage Pro2 weather station named "Davis-004" at Schiedam. The station is installed on the roof of the DCMR building, at a height of approx. 25 meters.This station is part of The Rotterdam Atmospheric Measurement Network (RAMN), funded with the help of TU Delft strategic funds, in collaboration with the Ruisdael Observatory.llaboration with the Ruisdael Observatory.)
TU Delft CMTRACE Level 1 Wind field at Cabauw + (Level 1 Data from the CMTRACE campaign at Cabauw.)

KNMI Lufft CHM 15k ceilometer at Cabauw + (Lufft CHM 15k ceilometer)

RITA22 - UUAQ-WUR Mobile Measurements + (Mobile measurements of several air pollutants made by a car in and around the city of Rotterdam during the RIT22 campaign.)
WUR Veenkampen meteorological and air quality observations + (Operationally, we measure meteorology, eva … Operationally, we measure meteorology, evaporation, CO2 exchange, soil variables and black carbon concentrations. Experimentally, we measure air quality concentrations and fluxes of NOx and NH3. The data documentation such as stream names, units and instrument type of the Veenkampen can be found in the Excelsheet at the website of https://maq-observations.nl/.e website of https://maq-observations.nl/.)
UU Proton transfer reaction mass spectrometer (PTR-MS) at Loobos + (Proton-transfer-reaction mass-spectrometer … Proton-transfer-reaction mass-spectrometer (PTR-MS) at the Loobos site (52°09'59.0"N 5°44'36.4"E). Ambient air is sampled through a ~50m PFA tubing (ID=6 mm, Flow ~10 L/min) from 30 m above the ground (~12 m above the forest canopy). The inlet is located next to a sonic anemometer and the full mass spectra are recorded at 2 Hz.he full mass spectra are recorded at 2 Hz.)
RITA 2021 + (Ruisdael Land-Atmosphere Interactions Intensive Trace-gas and Aerosol measurement campaign – Nitrogen and Aerosol Budget Closure experiment.)
PH-WUR aircraft measurements + (Ruisdael Loobos campaign, May 2022)
RITA 2022 + (Test how well the Ruisdael observatory can quantify urban emissions of air pollutants and greenhouse gases and their impacts.)
WUR Amsterdam urban meteorological and flux observations + (The Amsterdam Atmospheric Monitoring Super … The Amsterdam Atmospheric Monitoring Supersite (AAMS) contains an eddy covariance flux tower measuring turbulent fluxes of sensible heat, latent heat (evapotranspiration), CO2 and methane, and contains a scintillometer as well. Moreover, we measure up- and downwelling components of the solar and thermal radiation. The data documentation such as stream names, units and instrument type of the Veenkampen can be found in the Excelsheet at the website of https://maq-observations.nl/.e website of https://maq-observations.nl/.)
CINDI + (The CINDI campaign (Cabauw Intercomparison … The CINDI campaign (Cabauw Intercomparison Campaign of Nitrogen Dioxide measuring Instruments) is a CEOS, GEOMON and NDACC initiative. The main objective of this campaign is to intercompare the NO2 measuring instruments that can be used for validation of tropospheric NO2 from satellites. Many different in-situ and remote sensing instruments participated.d remote sensing instruments participated.)
TU Delft RPG-FMCW-DP-KW Cloud radar (CLARA) + (The cloud radar CLARA (CLoud Atmospheric R … The cloud radar CLARA (CLoud Atmospheric RAdar) is a dual-frequency (35 and 94 GHz) scanning polarimetric FMCW (Frequency Modulated Continuous Wave) radar, which profiles clouds and precipitation in the troposphere. The radar is located at KNMI's former Wind Profiler Site in Cabauw. Its specifications can be changed to address different measurement objectives. The maximum range is 12 km and the time, range and Doppler resolution are a few seconds, about 30 m and a few cm/s, respectively., about 30 m and a few cm/s, respectively.)
TU Delft RPG-FMCW-94-DP Cloud radar (LARA) + (The cloud radar LARA (Lutjewad Atmospheric … The cloud radar LARA (Lutjewad Atmospheric RAdar) is a 94 GHz scanning polarimetric FMCW (Frequency Modulated Continuous Wave) radar, which profiles clouds and precipitation in the troposphere. This cloud radar is located at Lutjewad Atmospheric Site. Its specifications can be changed to address different measurement objectives. The maximum range is 12 km and the time, range and Doppler resolution are a few seconds, about 30 m and a few cm/s, respectively., about 30 m and a few cm/s, respectively.)
TU Delft RPG-FMCW-94-DP Cloud radar (MARA) at Delft + (The cloud radar MARA (Mobile Atmospheric R … The cloud radar MARA (Mobile Atmospheric RAdar) is a 94 GHz scanning polarimetric FMCW (Frequency Modulated Continuous Wave) radar, which profiles clouds and precipitation in the troposphere. By default, the radar was placed at Green Village, Delft, when it did not participate to a campaign. Its specifications can be changed to address different measurement objectives. The maximum range is 12 km and the time, range and Doppler resolution are a few seconds, about 30 m and a few cm/s, respectively., about 30 m and a few cm/s, respectively.)
TU Delft RPG-FMCW-94-DP Cloud radar (MARA) + (The cloud radar MARA (Mobile Atmospheric R … The cloud radar MARA (Mobile Atmospheric RAdar) is a 94 GHz scanning polarimetric FMCW (Frequency Modulated Continuous Wave) radar, which profiles clouds and precipitation in the troposphere. By default, the radar is placed at KNMI's Remote Sensing Site in Cabauw, when it does not participate to a campaign. Its specifications can be changed to address different measurement objectives. The maximum range is 12 km and the time, range and Doppler resolution are a few seconds, about 30 m and a few cm/s, respectively., about 30 m and a few cm/s, respectively.)
TU Delft CMTRACE Level 2 Wind field at Cabauw + (The first field campaign from the Tracing … The first field campaign from the Tracing Convective Momentum Transport in Complex Cloudy Atmospheres experiment project (CMTRACE) took place in Cabauw, the Netherlands, between September 13th and October 3rd 2021. During this field campaign, two cloud radars and one wind lidar were operated with a similar scanning strategy for deriving wind speed and direction profiles from near the surface up to cloud tops. Here, we provide the daily Level 2 data from the campaign. At this level, several processing steps were applied to the original data from each instrument to minimize the differences between the sampled volumes and temporal and spatial resolution to generate merged profiles of wind speed and direction. Those processing steps are described in http://dx.doi.org/10.5194/essd-15-769-2023.'''Variables''':horizontal wind direction;horizontal wind speed;zonal wind;meridional wind;vertical wind speed;lidar relative beta;radar vertical doppler velocity;radar equivalent reflectivity;rain rate; radar equivalent reflectivity; rain rate;)
WUR atmospheric CO2, O2 and δ13CO2 dataset over a tropical and a temperate forest + (These are the datasets of the campaigns from CloudRoots and Loobos used in the paper titled 'Tracing diurnal variations of atmospheric CO2, O2 and δ13CO2 over a tropical and a temperate forest'.)
CINDI-3 + (Third Cabauw Intercomparison of Nitrogen D … Third Cabauw Intercomparison of Nitrogen Dioxide measuring Instruments, which took place at the Cabauw Experimental Site for Atmospheric Research (CESAR) from 21 May until 24 June 2024. CESAR is one of the main facilities of the Dutch Ruisdael Observatory located midway in between the cities of Rotterdam and Utrecht, and managed by KNMI.Over 100 researchers from 18 countries participated in CINDI-3, operating 32 UV-Vis DOAS instruments to compare and intercalibrate measurements of air pollutants and to support the validation of satellite measurements from space-borne instruments such as Sentinel-5p/TROPOMI. CINDI-3 is the third intercomparison campaign of this kind. The overall campaign planning and coordination was carried out by a steering committee, led by BIRA-IASB (Royal Belgian Institute for Space Aeronomy), coordinating the CINDI-3 intercomparison schedule and all additional activities such as the mobile and aircraft observations.The main science objectives of CINDI-3 are the following:- To assess the consistency of slant column measurements of several key target species (NO2, ozone, O4 and HCHO) of relevance for the validation of S5P and the future ESA atmosphericSentinels, through coordinated operation of a large number of DOAS and MAXDOAS instruments from all over the world.- To study the relationship between remote-sensing column- and profile-measurements of NO2, HCHO and ozone and reference in-situ concentration measurements of the same species.- To investigate the horizontal representativeness of MAXDOAS measuring systems in view of their use for the validation of satellite tropospheric measurements featuring ground pixel areas in the range of 25-50 km2.CINDI-3 was organized as part of the ACTRIS-CREGARS Topical Center for trace gas remote sensing, within the framework of the collaboration between ACTRIS and NDACC, and conducted with additional support from ESA, NASA and from the EU Horizon2020 ATMO-ACCESS project (https://www.atmo-access.eu/).Additionally, the campaign was supported by KNMI.The following instruments were used:- Static MAXDOAS and zenith-sky DOAS instruments- In situ ICAD instrument- Brewer- Ozone sondes- NO2 sondes- Lidar systems: The multiwavelength Raman lidar CAELI, UV-depolarisation lidar, Ceilometer, ESA EMORAL system, SMOL tropospheric ozone differential absorption lidar, NO2 differential absorption lidar, Mobile Aerosol Monitoring System (MAMS) and scanning AERONET photometer- Mobile DOAS instruments- Airborne measurements- Satellite data - Airborne measurements - Satellite data)
WUR CarbonTracker Europe CTE2024 fluxes + (This collection contains monthly and annua … This collection contains monthly and annual mean fluxes between 2001-2023 for the various components of the CarbonTracker Europe data assimilation system, for the inversions performed for the GCB2024.Prior biosphere fluxes are calculated using the SiB4 model (Haynes et al., 2019, https://doi.org/10.1029/2018MS001540). Prior ocean fluxes are taken from Jena Carboscope v2023 (Roedenbeck et al., 2013, https://doi.org/10.5194/os-9-193-2013). Imposed fire fluxes are taken from GFAS (di Giuseppe et al., 2018, https://doi.org/10.5194/acp-18-5359-2018). Imposed fossil fuel fluxes are taken from GridFED v2024.0 (Jones et al., 2021, https://doi.org/10.1038/s41597-020-00779-6).Please cite the paper of Friedlingstein et al., (2024, https://doi.org/10.5194/essd-2024-519) for the fluxes used. Please cite the paper of van der Laan-Luijkx et al., (2017, https://doi.org/10.5194/gmd-10-2785-2017) for the data assimilation system used.17) for the data assimilation system used.)
ACTRIS-EARLINET aerosol optical property profiles over CBW Cabauw - Netherlands + (This dataset collects all the aerosol opti … This dataset collects all the aerosol optical property profiles at the aerosol remote sensing CBW station (Cabauw - Netherlands). This dataset is incremental: data collected are added as soon as a new observation is collected and added to the ACTRIS/EARLINET database.Variables: Attenuated backscatter profile; Volume depolarization profile, Particle backscatter coefficient profile, Particle extinction coefficient profile, Lidar ratio profile, Ångström exponent profile, Backscatter-related Ångström exponent profile, Particle depolarization ratio profile.le, Particle depolarization ratio profile.)
KNMI DALES model outputs over Cabauw + (This dataset contains horizontally average … This dataset contains horizontally averaged statistics from unvalidated Dutch Atmospheric Large Eddy Simulation (DALES) forecasts with a lead time of 24h. The LES is ran using the Ruisdael branch of DALES (version 4.3) and are forced by HARMONIE 43. The domain with a horizontal extent of 15 km x 15 km and vertical range of 13.5 km is centred around Cabauw. The version of the unvalidated Ruisdael DALES can be accessed here: https://github.com/dalesteam/dales. The runs have a horizontal resolution of ~76m (in both directions) and a vertical resolution decreasing with height from 20 m to 150 m. Homogenous land cover is applied to the domain. Code can be accessed through: https://github.com/dalesteam/dales.'''Note:''' the latest version of the unvalidated Ruisdael DALES can be accessed here: https://github.com/dalesteam/dales. The runs have a horizontal resolution of ~76m (in both directions) and a vertical resolution decreasing with height from 20 m to 150 m. Homogenous land cover is applied to the domain.Bounding box is 51.7665 - 52.9013 N, 4.8167 - 5.0357 E is 51.7665 - 52.9013 N, 4.8167 - 5.0357 E)
WUR Loobos ecosystem historical data + (This is a 25 years (1996-2021) observation … This is a 25 years (1996-2021) observational dataset of meteorology, turbulent fluxes and net ecosystem exchange collected from the first tower at the Loobos site, the Netherlands (NL). The presented dataset contains six data streams, namely (1) the NL-Loo_BM stream including meteorological data: four-component radiation (radiation balance), air temperature and relative humidity, wind information, precipitation and throughfall, photosynthetic active radiation, bole temperature and soil heat flux), (2) the NL-Loo_Profile stream containing vertical profiles of CO₂ mole fraction, H₂O pressure, air temperature and relative humidity, (3) the NL-Loo_ST stream derived from the aforementioned two streams including total stored heat flux, H₂O and CO₂ fluxes below the canopy, (4) the NL-Loo_EC stream including EC measurements of CO₂ flux, sensible heat and latent heat fluxes, (5) the NL-Loo_Soil stream including vertical profiles of soil moisture and temperature and ground water level data, and (6) ancillary data including soil respiration, vegetation properties (i.e., tree height, stem width and dry aboveground biomass, Leaf Area Index, sap flow, needle foliage properties and the associated nutrient analysis) and ground water level. The data quality of these data streams is assured through standard operating procedures.red through standard operating procedures.)
TU Delft Micro Rain Radar MRR001 at Green Village + (Time-height profiles of precipitation by T … Time-height profiles of precipitation by TU Delft's Micro Rain Radar (MRR-PRO) manufactured by Metek GmbH. MRR001 is part of the Ruisdael mobile station and frequently changes location. When it is not used for field campaigns, the radar is placed at Green Village Delft. Time interval of measurements is 10 seconds with a range resolution of 35 meters, max range of 4480 meters and 64 Doppler spectral bins. The raw data are provided in the form of hourly NetCDF files.ovided in the form of hourly NetCDF files.)
TU Delft Micro Rain Radar MRR002 at Cabauw + (Time-height profiles of precipitation by T … Time-height profiles of precipitation by TU Delft's Micro Rain Radar (MRR-PRO) by Metek GmbH (SN 0512067699), placed at KNMI's Remote Sensing Site in Cabauw. Time interval of measurements is 10 seconds with a range resolution of 35 meters, max range of 4480 meters and 64 Doppler spectral bins. The raw data are provided in the form of hourly netCDF files.ovided in the form of hourly netCDF files.)
TNO INGOS Historic CH4 at 027m at Cabauw + (TNO INGOS Historic CH4 at 027m at Cabauw)
TNO INGOS Historic CH4 at 067m at Cabauw + (TNO INGOS Historic CH4 at 067m at Cabauw)
TNO INGOS Historic CH4 at 127m at Cabauw + (TNO INGOS Historic CH4 at 127m at Cabauw)
TNO INGOS Historic N2O at 027m at Cabauw + (TNO INGOS Historic N2O at 027m at Cabauw)