设为首页
加入收藏
Drought Changes in Southwest China and Its Impacts on Rice Yield of Guizhou Province
-
摘要: 近几年，我国西南地区干旱频繁发生，严重影响农业生产。为了探讨干旱和水稻产量之间关系的复杂性，采用中国气象局国家气象信息中心提供的西南地区348个站气象数据，计算了西南地区干旱的变化趋势，并利用2000—2011年贵州省县级水稻产量资料分析了干旱对水稻单产的影响，探讨了干旱、水资源灌溉以及水稻产量之间的关系。结果表明：1951—2012年西南地区降水量平均减少16.9 mm/10 a，特别是8—10月降水量明显减少。同时，西南地区干旱日数呈上升趋势，平均增加3.3 d/10 a。对比水稻产量发现，当累计干旱日数少于40 d时，干旱对水稻产量一般不会造成影响；当累计干旱日数超过86 d时，干旱造成水稻减产20%~73%，这意味着当累计干旱日数超过3个月时，江河塘库蓄水将受到影响，进而影响水稻的灌溉，造成水稻严重减产；当累计干旱日数为40~86 d时，水稻减产一般少于20%，但地区差异较大。Abstract: Extreme weather and climate events have become more frequent and severe in recent years in the context of global warming. These extreme events bring serious impacts on human survival and sustaining development of society. Drought is one of the major types of extreme climatic events in China, which seriously affects agriculture and social-economic development. The domestic extreme drought events in recent years mostly occur in Southwest China, influencing the agriculture severely. Using the high quality observations from 348 weather stations and the agriculture data of county level in Southwest China, the complicated relationship among droughts, water supply, and rice yields is investigated.The precipitation decreases in Southwest China from 1951 to 2012, with an average decadal decrease of 16.9 mm per 10 years. In particular, the precipitation decreases distinctly from August to October, mainly due to the weak South Asian monsoon. Drought days are counted by using the drought index ISWAP, and the result shows that the number of drought days generally increases by 3.3 days per 10 years in the past several decades, especially since 2001 due to the less precipitation. Since rice cultivation is irrigated agriculture, drought won't directly affect rice growth. To further understand the complexity, impacts of various drought events on rice yields are investigated using high quality rice yield data collected in 70 counties of Guizhou Province, and the result indicates that the drought has little adverse but favorable impacts on rice yields when annual accumulated number of drought days is less than 40 days. It is because that this kind of drought won't affect the rice irrigation water supply, and the temperature is usually abnormally high with more bright sunshine days during the period of drought which are actually favorable for rice growth. However, when the number of drought days is more than 86 days, rice yields will reduce by 20%-73% due to the drought and the insufficient irrigation. When the number of drought days is between 49-86 days, rice yields usually reduce by less than 20% but with large differences between different regions. This kind of drought has little impact on rice yields in regions of robust drought tolerance but greatly affects rice yields in regions of weak drought tolerance.
-
Key words:
- Southwest China;
- drought index;
- rice yield
-
图 1 我国西南地区具有1951—2012年数据序列的37个站 (a) 和具有1961—2012年序列的348个站 (b) 分布
Fig. 1 The distribution of 37 stations from 1951 to 2012 (a) and 348 stations from 1961 to 2012 (b) in Southwest China
图 2 1951—2012年我国西南地区年降水距平百分率 (a) 和8—10月降水量 (b) 变化
Fig. 2 The change of precipitation anomaly percentage (a) and the change of precipitation from Aug to Oct (b) from 1951 to 2012 in Southwest China
图 3 1951—2012年南亚夏季风指数变化
Fig. 3 The change of the South Asian summer monsoon index from 1951 to 2012
图 4 1951—2012年我国西南地区年干旱日数和生长季干旱日数变化
Fig. 4 The change of the number of annual drought days and the number of growing season drought days from 1951 to 2012 in Southwest China
图 5 2000—2011年贵州省县级水稻产量变化率及水稻生长季内累计干旱日数的关系
Fig. 5 The relationship between county rice yields and the number of drought days of growing season in Guizhou Province from 2000 to 2011
表 1 ISWAP等级划分
Table 1 The classification of ISWAP
等级 类型 ISWAP 1 无旱 -0.5 < ISWAP 2 轻旱 -1.0 < ISWAP≤-0.5 3 中旱 -1.5 < ISWAP≤-1.0 4 重旱 -2.0 < ISWAP≤-1.5 5 特旱 ISWAP≤-2.0 
下载: 导出CSV
表 2 2011年贵州省部分县水稻产量变化以及降水和干旱日数信息
Table 2 Changes of rice yields, precipitation and the number of drought days for some counties of Guizhou Province in 2011
县名 水稻产量变化幅度/% 4—9月降水量/mm 4—9月降水距平百分率/% 累计干旱日数/d 石阡 -72.9 336.1 -59.2 155 余庆 -67.7 456.8 -42.9 112 正安 -67.6 433.1 -47.4 102 黔西 -63.6 353.1 -53.5 136 水城 -60.4 559.7 -42.5 113 凤冈 -59.9 544.9 -39.9 117 德江 -58.5 597.2 -35.8 99 册亨 -57.1 524.6 -47.9 117 习水 -52.0 392.7 -52.2 140 开阳 -44.8 407.6 -51.6 147 毕节 -43.8 441.4 -37.2 127 金沙 -42.9 422.0 -46.8 115 安龙 -42.2 448.2 -53.7 141 榕江 -41.1 548.1 -37.6 100 锦屏 -39.0 546.2 -38.4 110 关岭 -38.9 712.4 -35.4 76 岑巩 -38.6 616.5 -24.7 92 福泉 -37.6 518.5 -40.7 111 贵定 -35.1 435.2 -49.7 142 独山 -34.5 519.5 -40.9 89 剑河 -31.3 556.8 -35.4 105 从江 -30.4 615.3 -29.8 68 长顺 -26.5 724.5 -33.8 93 赤水 -26.4 522.3 -41.4 107
下载: 导出CSV
-
[1] 联合国环境规划署 (UNEP). 全球环境展望. 北京: 中国环境科学出版社, 2000. [2] Changnon S A, Roger A, Pielke Jr, et al.Human factors explain the increased losses from weather and climate extremes.Bull Amer Meteor Soc, 2000, 81(3):437-442. doi: 10.1175/1520-0477(2000)081<0437:HFETIL>2.3.CO;2 [3] Easterling D R, Evans J L, Groismman P Y, et al.Observed variability and trends in extreme climate events:A brief review.Bull Amer Meteor Soc, 2000, 81(3):417-425. doi: 10.1175/1520-0477(2000)081<0417:OVATIE>2.3.CO;2 [4] 黄荣辉, 周连童.我国重大气候灾害特征、形成机理和预测研究.自然灾害学报, 2002, 11:1-9. doi: 10.3969/j.issn.1004-4574.2002.01.001 [5] 杨晓光, 李茂松.中国南方季节性干旱特征及种植制度适应.北京:气象出版社, 2014. [6] 傅伯杰.中国旱灾的地理分布特征与灾情分析.干旱区资源与环境, 1991, 5(4):1-8. http://www.cnki.com.cn/Article/CJFDTOTAL-GHZH199104000.htm [7] 顾颖, 刘静楠, 林锦.近60年来我国干旱灾害特点和情势分析.水利水电技术, 2010, 41(1):71-74. http://www.cnki.com.cn/Article/CJFDTOTAL-SJWJ201001022.htm [8] 国家气候中心. 全国气候影响评价2003. 北京: 气象出版社, 2003. [9] 中国气象局. 中国气象灾害年鉴. 北京: 气象出版社, 2007. [10] 中国气象局. 中国气象灾害年鉴. 北京: 气象出版社, 2011. [11] 中国气象局. 中国气象灾害年鉴. 北京: 气象出版社, 2012. [12] 中华人民共和国国家统计局. 2012中国统计年鉴. 北京: 中国统计出版社, 2013. [13] 刘德, 李永华, 高阳华, 等.重庆夏季旱涝的欧亚环流特征分析.高原气象, 2005, 24(2):275-279. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGQX200610004116.htm [14] 彭京备, 张庆云, 布和朝鲁.2006年川渝地区高温干旱特征及其成因分析.气候与环境研究, 2007, 12(4):464-474. http://www.cnki.com.cn/Article/CJFDTOTAL-QHYH200703025.htm [15] 李永华, 徐海明, 刘德.2006年夏季西南地区东部特大干旱及其大气环流异常.气象学报, 2009, 67(1):122-132. doi: 10.11676/qxxb2009.013 [16] 邹旭恺, 张强.近半个世纪我国干旱变化的初步研究.应用气象学报, 2008, 19(6):679-687. doi: 10.11898/1001-7313.20080607 [17] 于敏, 王春丽.不同卫星遥感指数在黑龙江的对比应用.应用气象学报, 2011, 22(2):221-231. doi: 10.11898/1001-7313.20110211 [18] 李剑锋, 张强, 陈晓宏, 等.基于标准化降水指标的新疆干旱特征演变.应用气象学报, 2012, 23(3):322-330. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20120308&flag=1 [19] 张存杰, 王宝灵, 刘德祥, 等.西北地区旱涝指标的研究.高原气象, 1998, 17(4):381-389. http://www.cnki.com.cn/Article/CJFDTOTAL-GYQX804.005.htm [20] 赵海燕, 高歌, 张培群, 等.综合气象干旱指数修正及在西南地区的适用性.应用气象学报, 2011, 22(6):698-705. doi: 10.11898/1001-7313.20110607 [21] Lu Er.Determining the start, duration, and strength of flood and drought with daily precipitation:Rationale.Geophys Res Let, 2009, 36: L12707, doi: 10.1029/2009GL038817. [22] 侯威, 杨杰, 赵俊虎.不同时间尺度下气象旱涝强度评估指数.应用气象学报, 2013, 24(6):695-703. doi: 10.11898/1001-7313.20130606 [23] Lu Er, Cai Wenyue, Jiang Zhihong, et al.The day-to-day monitoring of the 2011 severe drought in China.Clim Dyn, 2014, 43:1-9, doi: 10.1007/s00382-013-1987-2. [24] 张强, 邹旭恺, 肖风劲, 等. 气象干旱等级. GB/T20481—2006, 中华人民共和国国家标准. 北京: 中国标准出版社, 2006: 1-17. [25] Ren G, Ding Y, Zhao Z, et al.Recent progress in studies of climate change in China.Adv Atmos Sci, 2012, 29(5):958-977. doi: 10.1007/s00376-012-1200-2 [26] 张强, 潘学标, 马柱国, 等.干旱.北京:气象出版社, 2009:2-3. [27] 秦剑.气候因子与云南粮食生产的关系.应用气象学报, 2000, 11(2):213-220. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20000231&flag=1 [28] 中国气象局. 中国气象灾害年鉴. 北京: 气象出版社, 2003. -
计量
- 摘要浏览量: 4297
- HTML全文浏览量: 1121
- PDF下载量: 1120
- 被引次数: 0
