Resources Science ›› 2019, Vol. 41 ›› Issue (11): 2144-2153.doi: 10.18402/resci.2019.11.16
LIU Lin1,2, XU Zongxue2,3(), YANG Xiaojing2,3
Received:
2017-10-08
Revised:
2019-08-09
Online:
2019-11-25
Published:
2019-12-03
Contact:
XU Zongxue
E-mail:zxxu@bnu.edu.cn
LIU Lin, XU Zongxue, YANG Xiaojing. Relationship between drought/flood and ENSO events in Southwest China[J].Resources Science, 2019, 41(11): 2144-2153.
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Table 1
Intensity and grade of El Nino-Southern Oscillation (ENSO) events"
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 |
Table 2
Correlation between precipitation and sea surface temperature anomaly (SSTA) in El Nino-Southern Oscillation (ENSO) years during in Southwest China, 1960-2016"
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 |
Table 3
Correlation between temperature and sea surface temperature anomaly (SSTA) in ENSO years in Southwest China, 1960-2016"
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 |
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