GPS monitoring of the tropospheric water vapor distribution and variation during the 9 September 2002 torrential precipitation episode in the Cevennes (southern France) -: art. no. D24102

被引:63
作者
Champollion, C [1 ]
Masson, F
Van Baelen, J
Walpersdorf, A
Chéry, J
Doerflinger, E
机构
[1] Univ Montpellier 2, CNRS, Lab Dynam Lithosphere, F-34095 Montpellier, France
[2] Meteo France, CNRS, Ctr Natl Rech Meteorol, F-63006 Toulouse, France
[3] Univ Grenoble 1, CNRS, Lab Geophys Interne & Tectonophys, F-38041 Grenoble, France
关键词
GPS; water vapor; wet gradients; intense rainfall; integrated water vapor; residuals;
D O I
10.1029/2004JD004897
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
On 8-9 September 2002, torrential rainfall and flooding hit the Gard region in southern France causing extensive damages and casualties. This is an exceptional example of a so-called Cevenol episode with 24 hour cumulative rainfall up to about 600 mm at some places and more than 200 mm over a large area (5500 km(2)). In this work we have used GPS data to determine integrated water vapor (IWV) as well as horizontal wet gradients and residuals. Using the IWV, we have monitored the evolution of the convective system associated with the rainfall from the water vapor accumulation stage through the stagnation of the convective cell and finally to the breakup of the system. Our interpretation of the GPS meteorological parameters is supported by synoptic maps, numerical weather analyses, and rain images from meteorological radars. We have evidenced from GPS data that this heavy precipitation is associated with ongoing accumulation of water vapor, even through the raining period, but that rain stopped as soon as the weather circulation pattern changed. The evolution of this event is typical in the context of the Cevenol meteorology. Furthermore, we have shown that the horizontal wet gradients help describe the heterogeneity of the water vapor field and holds information concerning the passage of the convective system. Finally, we have noticed that the residuals, which in theory should be proportional to water vapor heterogeneity, were also highly perturbed by the precipitation itself. In our conclusions we discuss the interest of a regional GPS network for monitoring and for future studies on water vapor tomography.
引用
收藏
页码:1 / 15
页数:15
相关论文
共 31 条
[1]   ITRF2000: A new release of the International Terrestrial Reference frame for earth science applications [J].
Altamimi, Z ;
Sillard, P ;
Boucher, C .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2002, 107 (B10)
[2]  
[Anonymous], 2000, DOCUMENTATION GAMIT
[3]  
BARRON J, 1994, NEW STATESMAN SOC, V7, P38
[4]  
BOCK O, 2003, EGS AGU EUG JOINT AS
[5]  
Businger S, 1996, B AM METEOROL SOC, V77, P5, DOI 10.1175/1520-0477(1996)077<0005:TPOGIA>2.0.CO
[6]  
2
[7]  
CHAMPOLLION C, 2004, IN PRESS ATMOS RES
[8]   Effects of atmospheric azimuthal asymmetry on the analysis of space geodetic data [J].
Chen, G ;
Herring, TA .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1997, 102 (B9) :20489-20502
[9]   GEODESY BY RADIO INTERFEROMETRY - EFFECTS OF ATMOSPHERIC MODELING ERRORS ON ESTIMATES OF BASELINE LENGTH [J].
DAVIS, JL ;
HERRING, TA ;
SHAPIRO, II ;
ROGERS, AEE ;
ELGERED, G .
RADIO SCIENCE, 1985, 20 (06) :1593-1607
[10]  
DELRIEU G, 2004, IN PRESS J HYDROMETE