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CAMPAIGNS
Learn about the ground-based, ship-borne, balloon-borne, and airborne campaigns and small satellite field experiments that validate orbiting ESA EO satellites and support future mission development.
Campaign
DOMEX-3
The DOMEX-3 experiment is the follow on of two previous experiments called DOMEX-1 and DOMEX-2 which were successfully conducted at Concordia base, Antarctica
Campaign
PolarGap
The primary objective of the PolarGap campaign was to carry out an airborne gravity survey covering the southern polar gap of the gravity field mission GOCE, beyond the coverage of the GOCE orbit.
Campaign
CryoVExAnt 2014/2015
The aim of CryoVEx Ant 2014 to 2015 was to perform altimeter measurements at a designated validation site in the vicinity of the Schirmacher Oasis, near Kohnen and Neumayer as well as in the Pine Island Glacier drainage basin.
Campaign
SMOSice
The ESA SMOSice study has demonstrated for the first time the potential to retrieve sea ice thickness from SMOS data.
Campaign
CryoVEx AEM
CryoVEX 2014 performed measurements over the Beaufort Sea and Arctic Ocean north of Canada (Ellesmere Island) and Greenland. Airborne surveys and ground‐based snow and ice measurements were performed.
Campaign
DOMECair (SMOS)
The purpose of this campaign was to assess the merits of the East Antarctic Plateau around Dome C with the Concordia station as a candidate for an Earthly calibration site. It was an airborne campaign in Antarctica supporting SMOS calibration.
Campaign
DOMECair (GOCE)
The airborne survey DOMECair 2013 and its instrumentation was designed to obtain calibration and validation data for two different satellite missions of ESA’s Earth Explorer mission, for satellites SMOS and GOCE.
Campaign
CryoVExAnt 2010/2011
The CryoVEx 2010/2011 Antartic campaign was carried out in Dronning Maud Land from 11 November 2010 to 20 February 2011.
Campaign
CryoVEx 2011
The aims of the CryoSat Validation Experiment (CryoVEx) 2011 was to study the snow and ice characteristics of Arctic sea ice and its snow cover.
Campaign
DOMEX-2
The DOMEx-2 campaign is part of the calibration and validation activities of the SMOS mission, which is one of Earth Explorers within ESA's Living Planet programme.
Campaign
CoSMOS 2005, 2007, 2008, 2010
The Campaign for Validating the Operation of SMOS (coSMOS) was designed to acquire SMOS-like data so that the algorithms were fine-tuned and properly validated before the launch of SMOS mission in 2007.
Campaign
CryoVExAnt 2008/2009
The key objective of the CryoSat Validation Experiment Antarctica (CryoVExAnt) campaign is a better approximation of the error range of the elevation obtained from SAR-processed altimetric radar returns and its sensitivity to surface roughness.
Campaign
CoSMOS 2006
ESA conducted an airborne campaign to map sea surface salinity named "CoSMOS-OS" that took place in April 2006 over the Norway Sea off the coast of Stavenger.
Campaign
EAGLE
The general purpose of the EAGLE2006 campaign was: Acquisition of simultaneous multi-angular and multi-sensor (from visible to microwave domain) data over a grassland and a forest.
Campaign
DOMEX-1
The purpose of the DOMEX experiment was to acquire the first combined, in-situ microwave emission measurements using C- and L-band radiometers.
Campaign
CryoVEx 2003
The CryoVEx (CryoSat Validation EXperiment) 2003 campaign was a first comprehensive Arctic Ocean airborne and surface campaign, in support of the ESA satellite CryoSat, planned for launch late 2004.
Campaign
LOSAC
The L-band Ocean Salinity Airborne Campaign (LOSAC) objective is to understand the nature of the wind driven signatures in order to evaluate if corrections are necessary prior to salinity estimations based on the radiometer signals.
Campaign
ESAG
The European Survey of Arctic Gravity (ESAG) campaign objective was to acquire measurements of the Arctic Ocean, in support of GOCE mission; and acquire scanning laser ranging data and profiling laser altimetry over sea-ice north of Greenland.
Campaign
WISE
The objective of WInd and Salinity Experiment 2001 (WISE 2001) campaign was to get more data points and better wind speed measurements.