Vertical profiles of the aerosol particles hygroscopic properties, their mixing state as well as ...
Measuring evaporation (E) with lysimeters is costly and prone to numerous errors. By comparing th...
The El Niño-Southern Oscillation (ENSO) is the main driver of interannual climate extremes in Ama...
How would the spell of extreme weather observed over North America and western Europe during the ...
A global, monthly averaged time series of Sun-induced Fluorescence (SiF), spanning January 2007 t...
Aerosols directly affect the radiative balance of the Earth through the absorption and scattering...
Op 24 april was het precies een jaar geleden dat het KNMI het crowdsourcing initiatief WOW-NL lan...
Understanding how the overall risks of extreme events are changing in a warming world requires bo...
Empirical models, designed to predict surface variables over seasons to decades ahead, provide us...
The chlorine radical is a potent atmospheric oxidant, capable of perturbing tropospheric oxidativ...
Hg ∕ SO2, Hg ∕ CO, NOx ∕ SO2 (NOx being the sum of NO and NO2) emission ratios (ERs) in the plume...
The large-scale burning of crop residues in the North China Plain (NCP), one of the most densely ...
The European Organisation for the Exploitation of Meteorological Satellites (EUMETSAT) Ocean and ...
Independent observations can be used to diagnose and tune a data assimilation (DA) system. Analys...
This guide describes the data product files from the CMEMS KNMI Production Unit, what data servic...
This document describes the quality of the global ocean near-real-time daily L3 wind product (WIN...
We present a model description and benchmark evaluation of an extension of the tropospheric chemi...
Wind energy resource is subject to changes in climate. To investigate the impacts of climate chan...