The Impact of El Nino/Southern Oscillation on Hydrology and Rice Productivity in the Cauvery Basin, India: Application of the Soil and Water Assessment Tool

被引:31
作者
Bhuvaneswari, K. [1 ]
Geethalakshmi, V. [1 ]
Lakshmanan, A. [1 ]
Srinivasan, R. [2 ]
Sekhar, Nagothu Udaya [3 ]
机构
[1] Tamil Nadu Agr Univ, Agro Climate Res Ctr, Coimbatore 641003, Tamil Nadu, India
[2] Texas A&M Univ, Spatial Sci Lab, College Stn, TX USA
[3] Norwegian Inst Agr & Environm Res, Oslo, Norway
关键词
El Nino/Southern Oscillation; Cauvery River Basin; Soil and Water Assessment Tool; Hydrology; Rice Productivity;
D O I
10.1016/j.wace.2013.10.003
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
This study was performed to Further understanding of the variations in hydrology and rice crop productivity during different El Nino/Southern Oscillation (ENSO) events in the Cauvery River Basin of Tamil Nadu, India using the Soil and Water Assessment Tool (SWAT). The entire Cauvery Basin was divided into 301 sub-basins and further subdivided into 3,601 Hydrological Response Units (HRU). Based on the National Oceanic and Atmospheric Administration (NOAA) official website, information on El Nino (1972, 1982, 1987, 1991, 1997, 2002 and 2004) and La Nina (1970, 1971, 1973, 1974, 1975,1988, 1998, 1999 and 2000) years were obtained. The SWAT model was continuously run from 1970 to 2008, and a composite for El Nino, La Nina and normal years was constructed to understand their influence on hydrology and rice crop productivity in the study area. From the analysis, it was clear that an El Nino episode is correlated with rainfall, hydrology and rice productivity in the Cauvery river basin. The validation of the SWAT model indicated the capability of SWAT to accurately predict stream flow and rice productivity. It was evident from the investigation that the quantum of rainfall was more during El Nino years with high inter-annual rainfall variability (809.3 mm to 2,366 mm) compared with to Nina and normal years. As a result, the soil water recharge, including percolation and soil water availability in the surface layers, was increased in the El Nino years. Simulated rice productivity over 39 years in the Cauvery Basin ranged between 1,137 and 7,865 kg ha(-1) with a mean productivity of 3,955 kg ha(-1). The coefficient of variation in rice productivity was higher during La Nina (21.4%) years compared with El Nino (14.7%) and normal years (14.6%). The mean rice productivity was increased in both El Nino and normal years, indicating the possibility of higher yields than those in La Nina years. An analysis of the hydrological data and rice productivity showed that the risk of failure was low during El Nino years compared with normal or La Nina years. This behavior could be utilized for forecasting rice crop productivity under different ENSO conditions and can provide information for policy makers when deciding on water allocation and import / export policies. (C) 2013 The Authors. Published by Elsevier B.V.
引用
收藏
页码:39 / 47
页数:9
相关论文
共 28 条
[1]  
Annamalai H, 2007, J CLIMATE, V20, P1071, DOI 10.1175/JCL14035.1
[2]   Large area hydrologic modeling and assessment - Part 1: Model development [J].
Arnold, JG ;
Srinivasan, R ;
Muttiah, RS ;
Williams, JR .
JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION, 1998, 34 (01) :73-89
[3]   A COMPREHENSIVE SURFACE-GROUNDWATER FLOW MODEL [J].
ARNOLD, JG ;
ALLEN, PM ;
BERNHARDT, G .
JOURNAL OF HYDROLOGY, 1993, 142 (1-4) :47-69
[4]   Impact of ENSO and the Indian Ocean Dipole on the north-east monsoon rainfall of Tamil Nadu State in India [J].
Geethalakshmi, V. ;
Yatagai, Akiyo ;
Palanisamy, K. ;
Umetsu, Chieko .
HYDROLOGICAL PROCESSES, 2009, 23 (04) :633-647
[5]  
Geethalakshmi V., 2005, J METEOROL, V29, P9
[6]  
Hansen JW, 1998, J CLIMATE, V11, P404, DOI 10.1175/1520-0442(1998)011<0404:EIOAIT>2.0.CO
[7]  
2
[8]  
Hill HSJ, 1999, J CLIMATE, V12, P519, DOI 10.1175/1520-0442(1999)012<0519:TPIOTU>2.0.CO
[9]  
2
[10]   On the weakening relationship between the Indian monsoon and ENSO [J].
Kumar, KK ;
Rajagopalan, B ;
Cane, MA .
SCIENCE, 1999, 284 (5423) :2156-2159