The Argo Program has been implemented and sustained for almost two decades, as a global array of ...
This overview paper highlights the successes of the Ozone Monitoring Instrument (OMI) on board th...
A surface solar radiation forecast algorithm is developed using cloud physical properties from th...
The angular distribution of the light reflected by the Earth's surface influences top-of-atmosphe...
Aerosol-layer height is essential for understanding the impact of aerosols on the climate system....
The primary goal of this paper is to introduce two new surface reflectivity climatologies. The tw...
Accurate determination of radiative energy fluxes over the Arctic is of crucial importance for un...
Air mass factor (AMF) calculation is the largest source of uncertainty in NO2 and HCHO satellite ...
TEMPO was selected in 2012 by NASA as the first Earth Venture Instrument, for launch between 2018...
This paper presents an exploratory study on the aerosol layer height (ALH) retrieval from the OMI...
The Dutch–Finnish Ozone Monitoring Instrument (OMI) is an imaging spectrograph flying on NASA's E...
A key element in the assessment of seismic hazard and risk due to induced earthquakes in the Gron...
A community diagnostics and performance metrics tool for the evaluation of Earth System Models (E...
During LBA-CLAIRE-98, we found atmospheric layers with aged biomass smoke at altitudes >10 km ...
ERA-40 is a re-analysis of meteorological observations from September 1957 to August 2002 produce...
EBEX-2000 : the KNMI/WAU contribution
Environmental and climatic consequences of aviation: final report of the KNMI contributions to th...
The present report describes the results of an eight months working visit of M.H. at KNMI. The go...
GOME validation at KNMI and collaborating institutes
TEBEX observations of clouds and radiation - potential and limitations
Operational WAMS statistics over the period December 1986 - March 1987
Evaluatie van de golfberekeningen met GONO over de periode oktober 1985-april 1986
Evaluatie van de golfberekeningen met GONO over de periode oktober 1984 - april 1985