TROPOMI (Tropospheric Monitoring Instrument) onboard ESA’s Sentinel-5 Precursor satellite has bee...
. The direct radiative effect (DRE) of aerosols above clouds has been found to be significant ove...
The ultraviolet (UV) Absorbing Aerosol Index (AAI) is widely used as an indicator for the presenc...
The goal of the study described in this paper is to determine the accuracy of the radiometric cal...
This study presents an analysis of TROPOMI cloud heights as a proxy for volcanic plume heights in...
In this work, a ∼21-year global dataset from four different satellite sensors with a mid-morning ...
Retrievals of cloud properties from geostationary satellite sensors offer extensive spatial and t...
The retrieval of geophysical parameters is increasingly dependent on synergistic use of satellite...
The angular distribution of the light reflected by the Earth's surface influences top-of-atmosphe...
This paper presents a weighted least squares approach to retrieve aerosol layer height from top-o...
Retrieving aerosol optical thickness and aerosol layer height over a bright surface from measured...
Ozone profile retrieval from nadir-viewing satellite instruments operating in the ultraviolet–vis...
Absorbing aerosols exert a warming or a cooling effect on the Earth’s system, depending on the ci...
The primary goal of this paper is to introduce two new surface reflectivity climatologies. The tw...
Citizens are providing vast amounts of georeferenced data in the form of in situ data collections...
The Ozone Monitoring Instrument (OMI) is a push-broom imaging spectrometer, observing solar...
The three Global Ozone Monitoring Experiment-2 instruments will provide unique and long data sets...
An algorithm setup for the operational Aerosol Layer Height product for TROPOMI on the Sentinel-5...
Traditional validation of atmospheric profiles is based on the intercomparison of two or more dat...
In this paper we present validation results obtained from a direct comparison between the Absorbi...
Detecting the optical properties of aerosols using passive satellite-borne measurements alone is ...