西南地区旱涝演变与ENSO事件的关系

doi:10.18402/resci.2019.11.16

Abstract

Abstract:

Under the background of climate change, drought and flood occur frequently in Southwest China, and El Nino and Southern Oscillation (ENSO) is an important indicator of climate change. Based on the data of sea surface temperature anomaly (SSTA), Southern Oscillation Index (SOI), precipitation, and temperature during 1960-2016 in Southwest China, the correlation between ENSO events and precipitation, temperature, and drought/flood index was analyzed by using wavelet analysis and mathematical statistics. The results show that: (1) The ENSO events have quasi-periodic changes of about 9 a, 24 a, and 3~4 a. (2) There is a significant correlation between precipitation and ENSO event intensity, and temperature is also obviously correlated with ENSO event intensity, both with a certain lag of time. In the EI Nino event years, the precipitation and temperature in Southwest China are negatively correlated with SSTA with a lag of 2~4 months. In the La Nina event years, the precipitation and temperature in Southwest China are significantly positively correlated with SSTA with a lag of 2~4 months. The correlation between temperature and ENSO events is more obvious. (3) There was a negative correlation between the ENSO intensity and drought/flood grade. When the EI Nino event intensity increased, the number of drought events in the southwest region increased, and when the intensity of La Nina events increased, the number of flood events in the southwest region increased. The drought/flood index of Standardized Precipitation Index (SPI) and SOI also showed a very significant negative correlation, and the impact of ENSO on drought and flood had a lag of 1~4 months, with the greatest impact at 3 months lag. Therefore, drought and flood disasters are likely to occur in strong ENSO event years or the following year in the southwest region. This study may provide some reference for enhancing the vigilance against droughts/floods and strengthen flood control and drought relief work in Southwest China.

Key words: ENSO events, period, correlation, precipitation, temperature, drought/flood, Southwest China

LIU Lin, XU Zongxue, YANG Xiaojing. Relationship between drought/flood and ENSO events in Southwest China[J].Resources Science, 2019, 41(11): 2144-2153.

Figures/Tables 12

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References 33

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	起止年月	长度	等级	最强月份	最强季节	事件年
暖事件	1963.07—1964.01	7	1	1963.12	秋季	1963
	1965.07—1966.03	9	2	1965.10	秋季	1965
	1972.06—1973.02	9	3	1972.12	秋季	1972
	1982.05—1983.06	14	3	1982.12	冬季	1982—1983
	1986.09—1988.01	17	2	1987.09	秋季	1986—1987
	1991.06—1992.06	13	2	1992.01	冬季	1991
	1994.08—1995.02	7	2	1994.12	冬季	1994
	1997.05—1998.05	13	3	1997.11	秋季	1997
	2002.06—2003.02	9	2	2002.11	秋季	2002
	2004.07—2005.01	7	1	2004.09	秋季	2004
	2006.08—2007.01	6	1	2006.12	冬季	2006
	2009.07—2010.04	10	2	2009.12	冬季	2009
	2014.11—2016.04	18	3	2015.11	秋季	2015—2016
冷事件	1962.08—1963.02	7	-1	1963.01	冬季	1962
	1964.04—1965.02	11	-1	1964.09	秋季	1964
	1967.09—1968.05	9	-1	1968.02	冬季	1968
	1970.07—1972.02	20	-2	1971.01	冬季	1970—1971
	1973.05—1976.05	37	-3	1973.11	秋季	1974—1975
	1984.10—1985.09	12	-1	1984.12	冬季	1984
	1988.05—1989.06	14	-3	1988.11	秋季	1988
	1995.09—1996.03	7	-1	1995.11	秋季	1995
	1998.07—2001.02	32	-3	1999.01	冬季	1999—2000
	2007.08—2008.06	11	-2	2008.01	冬季	2007
	2010.07—2011.04	10	-2	2011.01	冬季	2010
	2011.08—2012.02	7	-1	2011.11	秋季	2011

ENSO事件类型	EI Nino		LA Nina
滞后期	Pearson相关性	显著性	Pearson相关性	显著性
同期	0.0144	0.8424	0.0369	0.6233
滞后1个月	-0.0835	0.2509	0.1298	0.0834
滞后2个月	-0.1575*	0.0299	0.1867*	0.0126
滞后3个月	-0.2014**	0.0055	0.2344**	0.0017
滞后4个月	-0.1965**	0.0069	0.2439**	0.0011
滞后5个月	-0.1295	0.0773	0.1833*	0.0152

ENSO事件类型	EI Nino		La Nina
滞后期	Pearson相关性	显著性	Pearson相关性	显著性
同期	-0.0098	0.8927	0.0120	0.8725
滞后1个月	-0.1418	0.0504	0.1750*	0.0191
滞后2个月	-0.2368**	0.0010	0.2906**	0.0001
滞后3个月	-0.2625**	0.0003	0.3154**	0.0000
滞后4个月	-0.2278**	0.0017	0.2625**	0.0004
滞后5个月	-0.1332	0.0691	0.1471	0.0521

时间	同期	滞后1个月	滞后2个月	滞后3个月	滞后4个月	滞后5个月
相关系数	-0.0387	-0.0920*	-0.0860*	-0.1302**	-0.0987*	-0.0574
显著性	0.3253	0.0193	0.0288	0.0009	0.0122	0.1463

Relationship between drought/flood and ENSO events in Southwest China

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