West African Monsoon observed with ground-based GPS receivers during African Monsoon Multidisciplinary Analysis (AMMA)

被引:65
|
作者
Bock, O. [1 ,10 ]
Bouin, M. N. [1 ]
Doerflinger, E. [2 ]
Collard, P. [2 ]
Masson, F. [9 ]
Meynadier, R. [10 ]
Nahmani, S. [1 ]
Koite, M. [7 ]
Balawan, K. Gaptia Lawan [4 ]
Dide, F. [3 ]
Ouedraogo, D. [12 ]
Pokperlaar, S. [13 ]
Ngamini, J. -B. [11 ]
Lafore, J. P. [8 ]
Janicot, S. [6 ]
Guichard, F. [5 ,8 ]
Nuret, M. [8 ]
机构
[1] IGN, LAREG, F-77455 Marne La Vallee 2, France
[2] Univ Montpellier 2, CNRS, UMR5243, Geosci Montpellier, F-34095 Montpellier 05, France
[3] Direct Natl Meteorol, Cotonou, Benin
[4] Direct Meteorol Niger, Niamey, Niger
[5] CNRS, URA1357, GAME, F-31057 Toulouse, France
[6] Univ Paris 06, LOCEAN, UMR7159, CNRS, F-75252 Paris, France
[7] Direct Natl Meteorol, Bamako, Mali
[8] Meteo France, CNRM, F-31057 Toulouse, France
[9] Univ Strasbourg, CNRS, UMR7516, IPGS, F-67084 Strasbourg, France
[10] Univ Paris 06, Serv Aeron, CNRS, UMR7620, F-75252 Paris 05, France
[11] ASECNA, Dakar, Senegal
[12] ASECNA, Ouagadougou 01, Burkina Faso
[13] Ghana Meteorol Agcy, Tamale, Ghana
关键词
D O I
10.1029/2008JD010327
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
A ground-based GPS network has been established over West Africa in the framework of African Monsoon Multidisciplinary Analysis (AMMA) in tight cooperation between French and African institutes. The experimental setup is described and preliminary highlights are given for different applications using these data. Precipitable water vapor (PWV) estimates from GPS are used for evaluating numerical weather prediction (NWP) models and radiosonde humidity data. Systematic tendency errors in model forecasts are evidenced. Correlated biases in NWP model analyses and radiosonde data are evidenced also, which emphasize the importance of radiosonde humidity data in this region. PWV and precipitation are tightly correlated at seasonal and intraseasonal timescales. Almost no precipitation occurs when PWV is smaller than 30 kg m(-2). This limit in PWV also coincides well with the location of the intertropical discontinuity. Five distinct phases in the monsoon season are determined from the GPS PWV, which correspond either to transition or stationary periods of the West African Monsoon system. They may serve as a basis for characterizing interannual variability. Significant oscillations in PWV are observed with 10- to 15-day and 15- to 20-day periods, which suggest a strong impact of atmospheric circulation on moisture and precipitation. The presence of a diurnal cycle oscillation in PWV with marked seasonal evolutions is found. This oscillation involves namely different phasing of moisture fluxes in different layers implying the low-level jet, the return flow, and the African Easterly Jet. The broad range of timescales observed with the GPS systems shows a high potential for investigating many atmospheric processes of the West African Monsoon.
引用
收藏
页数:22
相关论文
共 50 条
  • [41] ECOCLIMAP-II: An ecosystem classification and land surface parameters database of Western Africa at 1 km resolution for the African Monsoon Multidisciplinary Analysis (AMMA) project
    Kaptue, Tchuente Armel Thibaut
    Roujean, Jean-Louis
    Faroux, Stephanie
    REMOTE SENSING OF ENVIRONMENT, 2010, 114 (05) : 961 - 976
  • [42] Analysis of Low-Level Atmospheric Moisture Transport Associated with the West African Monsoon
    Lele, M. Issa
    Leslie, Lance M.
    Lamb, Peter J.
    JOURNAL OF CLIMATE, 2015, 28 (11) : 4414 - 4430
  • [43] A Boundary Forcing Sensitivity Analysis of the West African Monsoon Simulated by the Modele Atmospherique Regional
    Chagnaud, Guillaume
    Gallee, Hubert
    Lebel, Thierry
    Panthou, Geremy
    Vischel, Theo
    ATMOSPHERE, 2020, 11 (02)
  • [44] Analysis of the West African Monsoon system in the regional climate model COSMO-CLM
    Kothe, S.
    Luethi, D.
    Ahrens, B.
    INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2014, 34 (02) : 481 - 493
  • [45] Model Simulations of Complex Dust Emissions over the Sahara during the West African Monsoon Onset
    Cavazos-Guerra, Carolina
    Todd, Martin C.
    ADVANCES IN METEOROLOGY, 2012, 2012
  • [46] Weakening and Shifting of the Saharan Shallow Meridional Circulation during Wet Years of the West African Monsoon
    Shekhar, Ravi
    Boos, William R.
    JOURNAL OF CLIMATE, 2017, 30 (18) : 7399 - 7422
  • [47] Understanding the Mechanisms behind the Northward Extension of the West African Monsoon during the Mid-Holocene
    Gaetani, Marco
    Messori, Gabriele
    Zhang, Qiong
    Flamant, Cyrille
    Pausata, Francesco S. R.
    JOURNAL OF CLIMATE, 2017, 30 (19) : 7621 - 7642
  • [48] Interdecadal variation of the West African summer monsoon during 1979-2010 and associated variability
    Li, Huanlian
    Wang, Huijun
    Yin, Yizhou
    CLIMATE DYNAMICS, 2012, 39 (12) : 2883 - 2894
  • [49] Simulations of the observed 'jump' in the West African monsoon and its underlying dynamics using the MIT regional climate model
    Im, Eun-Soon
    Eltahir, Elfatih A. B.
    INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2018, 38 (02) : 841 - 852
  • [50] Dynamics of the West African Monsoon. Part IV: Analysis of 25-90-Day Variability of Convection and the Role of the Indian Monsoon
    Janicot, Serge
    Mounier, Flore
    Hall, Nicholas M. J.
    Leroux, Stephanie
    Sultan, Benjamin
    Kiladis, George N.
    JOURNAL OF CLIMATE, 2009, 22 (06) : 1541 - 1565