Assessment of different precipitation datasets and their impacts on the water balance of the Negro River basin

被引:63
作者
Getirana, A. C. V. [1 ,2 ]
Espinoza, J. C. V. [3 ,4 ]
Ronchail, J. [5 ]
Rotunno Filho, O. C. [1 ]
机构
[1] Univ Fed Rio de Janeiro, Programa Engn Civil, Rio De Janeiro, Brazil
[2] Univ Toulouse, UPS OMP, IRD, LEGOS, Toulouse, France
[3] Inst Geofis Peru, Lima, Peru
[4] Univ Agr La Molina, Lima, Peru
[5] Univ Paris 07, LOCEAN IPSL, Paris, France
关键词
Water balance; Precipitation dataset; Hydrological modeling; Negro River basin; Amazon River basin; GLOBAL PRECIPITATION; SURFACE-WATER; RAINFALL VARIABILITY; ANALYSIS TMPA; AMAZON BASIN; NCEP-NCAR; MODEL; PRODUCTS; PROJECT; ERA-40;
D O I
10.1016/j.jhydrol.2011.04.037
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
With the objective of understanding the potential and limitations of available precipitation products for hydrological studies, this paper compares six daily and sub-daily precipitation datasets and their impacts on the water balance of the Negro River basin in the Amazon basin. The precipitation datasets contain gauge-based data [data derived from the Hybam Observatory Precipitation (HOP) dataset and provided by the Climate Prediction Center (CPC)], satellite-based data [the Global Precipitation Climatology Project (GPCP) one-degree daily and TRMM Multisatellite Precipitation Analysis (TMPA) datasets] and model-based data [the NCEP-DOE AMIP-II re-analysis (NCEP-2) and 40-year ECMWF Re-Analysis (ERA-40) datasets]. Each dataset has a common set of meteorological forcing data which are used to run the MGB-IPH hydrological model for the period from January 1998 to August 2002. The average precipitation of all the datasets is 2542 mm for the Negro River basin, with a standard deviation of 317 mm. TMPA and NCEP-2 have the lowest (2216 mm/year) and the highest (3065 mm/year) precipitation rates, respectively. The HOP and CPC datasets agree best with observed discharge. GPCP gives the best results among the ungauged datasets, followed by ERA-40. TMPA and NCEP-2 are found to be the least accurate. TMPA can reproduce the water cycles reasonably well, but underestimates the precipitation fields and discharges over the basin, while NCEP-2 is unable to represent the rainfall quantity and cycles, and the water discharge. Results suggest that gauge-based data are still the most representative of the actual precipitation in the northern Amazon basin. However, some satellite and model-based can reproduce fairly well the water cycle at the basin scale and monthly time step. (C) 2011 Elsevier B.V. All rights reserved.
引用
收藏
页码:304 / 322
页数:19
相关论文
共 87 条
[1]   Adjustment of global gridded precipitation for systematic bias [J].
Adam, JC ;
Lettenmaier, DP .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2003, 108 (D9)
[2]  
Adler RF, 2001, B AM METEOROL SOC, V82, P1377, DOI 10.1175/1520-0477(2001)082<1377:IOGPPT>2.3.CO
[3]  
2
[4]  
Adler RF, 2003, J HYDROMETEOROL, V4, P1147, DOI 10.1175/1525-7541(2003)004<1147:TVGPCP>2.0.CO
[5]  
2
[6]  
Allasia DG, 2006, IAHS-AISH P, V303, P360
[7]  
[Anonymous], 2008, CLIMATOLOGIE, DOI DOI 10.4267/CLIMATOLOGIE.746
[8]  
[Anonymous], NATO ASI SERIES 1
[9]  
[Anonymous], 1993, HDB HYDROL
[10]   Hydrometeorology of the Amazon in ERA-40 [J].
Betts, AK ;
Ball, JH ;
Viterbo, P ;
Dai, A ;
Marengo, J .
JOURNAL OF HYDROMETEOROLOGY, 2005, 6 (05) :764-774