Validation of the SST-dependent Ku-band geophysical model function for SCATSAT-1 scatterometer | ...
The Aeolus Data Innovation and Science Cluster (DISC) supports the Aeolus mission with a wide ran...
The time scales of the Paris Climate Agreement indicate urgent action is required on climate poli...
There is a general lack of information about the potential effects of 1.5, 2 or more degrees of g...
Attributing the change in likelihood of extreme weather events, particularly those occurring at s...
Northeast Brazil experienced profound water shortages in 2016 due to a five-year drought. Using m...
Deforestation and draining of the peatlands in equatorial SE Asia has greatly increased their fla...
This article explores the use of the ensemble Kalman filter technique to improve the accuracy of ...
In a warmer climate, it is expected that precipitation intensities will increase and form a consi...
Mercury was measured onboard the IAGOS-CARIBIC passenger aircraft from May 2005 until February 20...
Nitrogen dioxide (NO2) and formaldehyde (HCHO) column data from satellite instruments are used fo...
The seismic hazard and risk analysis for the onshore Groningen gas field requires information abo...
In this study, we investigated the role of climatic variability and atmospheric nitrogen depositi...
The sea-surface winds from the RapidScat scatterometer (RSCAT) onboard the International Space St...
The second-generation exploitation of meteorological satellite polar system (EPS-SG) C-band-wavel...
The assimilation of Advanced Scatterometer (ASCAT) winds has proven to be beneficial for the Euro...
Local systematic differences between scatterometer and global numerical weather prediction (NWP) ...
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...