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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
CLARE
CLARE 2000: Cloud Lidar and Radar Experiments were to provide an extended data base and develop new analysis methods.
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
LaRA
To improve our knowledge of how best to measure ice thickness, the airborne Laser and Radar Altimeter campaign (LaRA) was carried out over the frozen expanses of northern Greenland.
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
SPARC
ESA's SPectra bARrax Campaign (SPARC) activity was part of the preparatory study for a proposed ESA Earth Explorer mission called SPECTRA. The objective was to collect a CHRIS/PROBA reference dataset for SPECTRA-related studies.
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 2004
CryoVex 2004 was the second combined airborne and surface campaign for the preparation of the CryoSat mission, after successful completion of CryoVex 2003 by DTU.
Campaign
CryoVEx 2005
CryoVEx 2005 was the third combined airborne and surface campaign for the preparation of the CryoSat mission. It followed the 2004 campaign, which first utilised the new ASIRAS radar.
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
CryoVEx 2006
CryoSat Validation Experiment (CryoVEx) 2006 was carried out between 18 April and 18 May 2006 in the Arctic.
Campaign
BioSAR 2007
The BioSAR campaign aimed to support geophysical algorithm development, calibration/validation and the simulation of future spaceborne Earth Observation missions.
Campaign
IceSAR 2007
The objectives of IceSAR 2007 campaign was to acquire SAR images and complementary data over sea and land ice for preparation of Sentinel-1 mission and for providing a basis for the assessment of potential applications of Biomass mission.
Campaign
CEFLES2
The objective of the CEFLES2 campaigns was to provide key reference data and background knowledge for the preparatory phases of the Sentinel‐2 and FLEX missions.
Campaign
CryoVEx 2007
Following the successful 2004, 2005 and 2006 campaigns, the CryoVEx2007 campaign took place in Svalbard from 15 to 25 April 2007.
Campaign
BioSAR 2008
The main objective of BioSAR-2 (BioSAR 2008) campaign was to record SAR data over boreal forests with topographic effects to investigate the effect on biomass retrieval.
Campaign
POLARIS Proof of Concept 2008
The POLARIS Proof-of-Concept (PoC) 2008 campaign primarily aimed to verify the usefulness of the system for glaciological applications.
Campaign
CryoVEx 2008
The ESA CryoSat Validation Experiment, CryoVEx 2008 was carried out in April and May 2008.
Campaign
AgriSAR 2009
The AgriSAR 2009 campaign was defined to leverage the RADARSAT-2 mission to better understand and demonstrate the potential for GMES land monitoring user services, particularly in agriculture.
Campaign
POLARIS - Proof of Concept 2009
POLARIS - Proof of Concept (PoC) 2009 is a follow on campaign from POLARIS - PoC 2008. It focused on an additional POLARIS test with the objective to system test after system upgrade and the acquisition of fully polarimetric data of glaciological interest.
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.