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Recent improvements in the E-OBS gridded data set for daily mean wind speed over Europe in the period 1980--2021
In this work, we present the most recent updates in the E-OBS gridded data set for daily mean win...
Jouke H. S. de Baar, Linh Nhat Luu, Gerard van der Schrier, Else J. M. van den Besselaar, and Irene Garcia-Marti | Journal: Advances in Science and Research | Volume: 20 | Year: 2023 | First page: 91 | Last page: 95 | doi: https://doi.org/10.5194/asr-20-91-2023
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Beter bijtijds buien monitoren - Het vernieuwde realtimeneerslagproduct van het KNMI
Nauwkeurige, tijdige en gedetailleerde neerslaginformatie is essentieel voor het waterbeheer en v...
Aart Overeem, Hidde Leijnse, Mats Veldhuizen, Bastiaan Anker, Tim Vlemmix, Rik Noorlandt, Tim den Dulk, Jouke Jacobi, Ben Lankamp met illustraties van Frédérik Ruys (KNMI) | Journal: Meteorologica | Volume: 34 | Year: 2025 | First page: 16 | Last page: 22
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Recent improvements in spatial regression of climate data
Climate and weather services rely, for a large part, on data obtained from in situ measurement st...
Jouke de Baar, Irene Garcia-Marti | Journal: NATOAVT-354 workshop on multi-fidelity methods for military vehicle design | Year: 2022 | doi: http://dx.doi.org/10.13140/RG.2.2.25417.52325
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"Come as you are": Reconsidering the need for complex quality control when gridding crowd-sourced weather data
Recording hourly-mean in situ observations of surface air temperature is a core task of most Nati...
Jouke de Baar, Gerard van der Schrier | Journal: Quarterly Journal of the Royal Meteorological Society | Volume: n/a | Year: 2024 | First page: 1 | Last page: 17 | doi: https://doi.org/10.1002/qj.4890
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Spatial regression of multi-fidelity meteorological observations using a proxy-based measurement error model
High-resolution weather maps are fundamental components of early warning systems, since they
ena...
Jouke H. S. de Baar, Irene Garcia-Marti, Gerard van der Schrier | Journal: Advances in Science & Research | Year: 2023 | doi: https://doi.org/10.5194/asr-20-49-2023
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