FN Archimer Export Format PT J TI SSM/I integrated water vapor content measurements in coastal regions: A comparison with shipborne and airborne remote sensing measurements, radiosonde measurements, and NWP model retrievals - art. no. 8056 BT AF FLAMANT, C PELON, J EYMARD, L TOURNADRE, Jean AS 1:;2:;3:;4:; FF 1:;2:;3:;4:PDG-DRO-DOPS-LOS; C1 Univ Paris 06, Serv Aeron, IPSL, CNRS, F-75252 Paris, France. Univ St Quentin Versailles, CNRS, IPSL, Ctr Etud Environm Terr & Planetaires, F-78140 Velizy Villacoublay, France. IFREMER, Dept Oceanog Spatiale DRO OS, F-29280 Plouzane, France. C2 UNIV PARIS 06, FRANCE UNIV ST QUENTIN VERSAILLES, FRANCE IFREMER, FRANCE SI BREST SE PDG-DRO-DOPS-LOS IN WOS Ifremer jusqu'en 2018 copubli-univ-france IF 2.992 TC 7 UR https://archimer.ifremer.fr/doc/00000/10184/7733.pdf LA English DT Article DE ;SSM/I;Lidar;microwave radiometry;integrated water vapor content;Mistral;FETCH AB [1] The Special Sensor Microwave Imager (SSM/I) integrated water vapor content (IWVC) estimates in a coastal region during nonstationary cold-air outbreak conditions are analyzed using IWVC retrievals obtained from shipborne microwave radiometry (DRAKKAR), water vapor differential absorption laser remote sensing (LEANDRE 2), radiosonde measurements, and numerical weather prediction (NWP) model ALADIN of Meteo-France. The study focuses on the 24 March 1998 Tramontane/Mistral event, which occurred over the Gulf of Lion (GoL) (western Mediterranean) in the framework of the flux, etat de mer et teledetection en condition de fetch variable (FETCH) experiment. Comparisons of SSM/I and ALADIN IWVCs with collocated shipborne microwave radiometry, at distances from the coast between 50 and 100 km, were carried out on a full diurnal cycle. In the morning, when moister conditions prevailed, the agreement between SSM/I (one passage) and DRAKKAR was good while the bias observed in the afternoon (three passages) was larger (i.e., 2 kg m(2)). Reasons for this are investigated. We show that this is due to the fact that the sensitivity limit of the algorithm has been reached during very dry Mistral conditions. This bias is not explained by effects of land contamination, which is shown to remain below 0.2 kg m(-2). No systematic bias was observed between ALADIN and DRAKKAR. Nevertheless, the trend observed on the DRAKKAR data between 1430 and 2030 UT was best captured by SSM/I despite the sensitivity issue. SSM/I and ALADIN IWVC estimates were also found to be in good agreement with collocated airborne lidar measurements, thereby reproducing the spatial evolution of the IWVC with the distance to the coast. PY 2003 SO Journal Of Geophysical Research Oceans SN 0148-0227 PU Amer Geophysical Union VL 108 IS C3 UT 000181568200001 DI 10.1029/2001JC001068 ID 10184 ER EF