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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
WaddenSAR
The “WaddenSAR – Airborne bistatic C-band SAR experiment to demonstrate different acquisition geometries” was initiated to support the development of the Earth Explorer 10 Harmony mission.
Campaign
SnowSum
The SnowSum experiment is designed to support the development of future concepts to monitor the cryosphere.
Campaign
CIMREx
CIMREx airborne campaign aimed to sample the sea ice microwave emissions from various sea ice regimes around Svalbard and Greenland.
Campaign
WindVal III
The objectives the WindVal III campaign were derived from results, experience and lessons learnt of the last airborne campaigns in 2009, 2015 and 2016.
Campaign
Sentinel-3 OLCI Tandem 2018
In 2018, a tandem campaign was conducted between the Sentinel-3A and 3B satellites to help test the future FLEX mission.
Campaign
Drift4SKIM
As part of the detailed design and feasibility studies of the Sea Surface Kinematics Multiscale (SKIM) 9th Earth Explorer program candidate mission, ESA initiated the Drift4SKIM field campaign, with the aim to evaluate the feasibility of measuring the insitu Total Surface Current Velocity (TSCV) using pulse-pair Doppler radars.
Campaign
CryoVEx KAREN 2017
The CryoVEx-KAREN 2017 Campaign in the Arctic had the goal to collect unique measurements to help us better understand how sea ice is changing.
Campaign
CryoVEx 2016 Spring
The CryoVEx 2016 campaign was primarily carried out to follow up on a recommendation given within ESA CryoVal Land Ice project (2014-2015), where it was found that the traditional under-flights of the CryoSat-2 satellite were inadequate.
Campaign
GWEX
The aim of this study was to perform Gravity Wave (GW) observations with the airborne IRLI GLORIA on board of HALO. In this way for a first time 3-D tomographic reconstructions of mesoscale GW events in the lower stratosphere were taken.
Campaign
WindVal II
The objectives for the WindVal II campaign in 2016 were derived from the results, experience and lessons learnt from these last airborne campaigns in 2009 and 2015.
Campaign
CryoVEx KAREN 2016 Fall
The CryoVEx-KAREN 2016 Fall Campaign in Ilulissat, Greenland had the goal to collect unique measurements to help us better understand how snow and ice on the Greenland ice sheet is changing over time, and help ESA design future space missions to monitor the changing climate in our polar regions.
Campaign
EPATAN 2016
The main scientific objectives of EPATAN 2016 (Earthcare PrepAraTion cAmpaigN) were derived from the scientific objectives of EarthCARE.
Campaign
AROMAT-II
This campaign covers the fields of atmospheric composition: NO2, SO2, aerosols, over Romania (Bucharest and Turceni) and Germany (Berlin).
Campaign
WindVal I
The objectives of the WindVal 1 campaign in 2015 were derived from results, experience and lessons learnt from the previous airborne campaign in 2009.
Campaign
AirScatterGNSS
In this project an Airborne Wind Vector Scatterometer (AWVS) system was designed and built for measurements of sea surface backscattering from an aircraft.
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
CryoVEx ASIRAS 2014
The CryoVEx 2014 airborne campaign was conducted as two separate operational periods. The sea ice activities covering large parts of the western Arctic Ocean were planned to take place early in the season to make sure the weather was stable.
Campaign
COMEX
The COMEX campaign supports the mission definition of CarbonSat and HyspIRI by providing representative airborne remote sensing data ‐ MAMAP for CarbonSat.
Campaign
CHARADMexp
The ESA CHARADMExp campaign focuses on marine and marine-dust aerosol mixture characterisation.
Campaign
AROMAT-I
The main objective of this AROMAT-I campaign was to test newly developed airborne sensors and to evaluate their capabilities as validation tools for future air quality space borne sensors, in particular TROPOMI.