| 树轮记录的吉尔吉斯斯坦东部过去百年干湿变化 |
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| 引用本文： | 张瑞波,袁玉江,魏文寿,何清,尚华明,张同文,ERMENBAEV Bakytbek,赵勇.树轮记录的吉尔吉斯斯坦东部过去百年干湿变化[J].干旱区地理,2013,36(4):691-699. |
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| 作者姓名： | 张瑞波 袁玉江 魏文寿 何清 尚华明 张同文 ERMENBAEV Bakytbek 赵勇 |
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| 作者单位： | 1.中国气象局乌鲁木齐沙漠气象研究所；中国气象局树轮年轮理化研究重点开放实验室；新疆树木年轮生态实验室，新疆 乌鲁木齐 830002； 2 吉尔吉斯斯坦国家科学院水问题与水能研究所，吉尔吉斯斯坦，比什凯克，720033 |
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| 基金项目： | 国家国际科技合作计划项目（2010DFA92720-14）；国家自然科学基金（41071072）共同资助 |
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| 摘 要： | 利用吉尔吉斯斯坦东部chon-kyzyl-suu附近的两个树轮宽度年表，与CRU气温、降水资料和PDSI资料进行相关分析和响应分析，重建该地区过去百年的降水和PDSI，分析近百年吉尔吉斯斯坦东部干湿变化特征。结果表明：（1）该地区树轮宽度对降水和PDSI响应较好，利用树轮宽度年表可以较好地重建该地区过去百年上年7月到当年6月的降水和PDSI序列；（2）近百年该地区干湿变化具有明显的6 a、13 a和21 a左右的变化准周期；在1913年前后、1943年前后和1972年前后发生了由多到少的气候突变，在1950年前后发生了由少到多的气候突变；（3）吉尔吉斯斯坦东部过去百年干湿变化与中国境内天山山区降水变化一致：1890s偏干，1900s是最为湿润的10 a，1910s是最为干旱的10 a，1917年是近百年来最干旱的1 a，1920s-1930s偏湿，1940s偏干，1950s-1960s偏湿，1970s偏干，1980s-2000s偏湿，尤其是1980年以后到现在，天山山区经历了近百年最为漫长的增湿期；重建的近百年吉尔吉斯斯坦东部干湿变化能较好的代表西天山大部分区域尤其是西天山北坡吉尔吉斯斯坦境内的干湿变化。
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| 关 键 词： | 吉尔吉斯斯坦 树木年轮 降水 PDSI 气候变化 |
| 收稿时间： | 2012-12-04 |
Changes of wet and dry in the past hundred years in eastern Kyrgyzstan by tree-ring |
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| ZHANG Rui-bo,YUAN Yu-jiang,WEI Wen-shou,HE Qing,SHANG Huang-ming,ZHANG Tong-wen,ERMENBAEV Bakytbek,ZHAO Yong.Changes of wet and dry in the past hundred years in eastern Kyrgyzstan by tree-ring[J].Arid Land Geography,2013,36(4):691-699. |
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| Authors: | ZHANG Rui-bo YUAN Yu-jiang WEI Wen-shou HE Qing SHANG Huang-ming ZHANG Tong-wen ERMENBAEV Bakytbek ZHAO Yong |
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| Abstract: | The Western Tianshan Mountains in Kyrgyzstan，which is one of the most important water source area，is dominated by westerly and plays an important role in global change research. It is vital to understand the fact of past precipitation changes and explore its possible influence mechanism to the sustainable utilization of regional water resources. Because it is located in the arid inland area，tree rings are sensitive to moisture status and is a good proxy of past precipitation. In this paper，the tree-ring samples of Schrenk spruce （Picea schrenkiana Fisch.] et Mey） were collected from the upper and lower treeline of chon-kyzyl-suu on the western Tianshan，Kyrgyzstan in 2012，were used to develop two tree-ring width chronolgies using standard dendrochronological methods. The smoothing spline（SPL），negative exponential curve（NEP） and regional curve（RCS） method were used for removing the growth trend. Finally，standard chronology （STD），residual chronology（RES） and ARSTAN chronology （ARS） were obtained. The similarities and differences were analyzed of tree-ring response to climate between upper and lower treeline using Climatic Research Unit （0.5°×0.5°） and Palmer Drought Severity Index （2.5°×2.5°）. Single correlation calculation indicated that there are a best response between tree-ring width standard chronology and precipitation，and a better response between tree-ring chronology and Palmer Drought Severity Index. The correlation coefficient between KZX tree-ring width standard chronology（SPL） and precipitation from previous July to current June in eastern Kyrgyzstan was 0.61 （p]<]0.000 001）. The precipitation and Palmer Drought Severity Index that from previous July to current June over past hundred year were reconstructed using tree ring width chronologies. The model passed all the calibration by the leave-one-out cross-validation method. The power spectrum analysis and morlet wavelet transform reveals that wet and dry spells change with the quasi-periodic 6 a，13 a and 21 a in eastern Kyrgyzstan over the past hundred years. The oscillations were more strong from 1880s to 1920s，the periodic oscillation was significantly reduced in late 20th century，especially after 1980，and change cycles of 13 a and 21 a were most obvious in 1920-1980. The cycles implies that wet and dry changes in the past century in eastern Kyrgyzstan not only contain the local information，but also were impacted by a wider climate change，and the global climate change was further proved. The sliding T-test shows that there were 4 abrupt changes in 1913，1943，1972 and 1950. The dry and wet changes were consistent between the eastern Kyrgyzstan and the Tianshan Mountain in China over the past hundred years：It was dry in 1890s，wettest in 1900s，driest decade in 1910s，driest year in 1917，then the precipitation increased from 1920s to 1930s，dry in 1940s，wet from 1950s to 1960s，dry in 1970s，and wet from 1980s to 2000s，especially from 1980 to the present，which was the longest wet period for the past 100 years. Reconstruction sequence could better reflect the wet and dry change in most areas of the Western Tianshan Mountains，especially on the northern slope of the Tianshan Mountains in Kyrgyzstan. |
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| Keywords: | Kyrgyzstan Tree-ring Precipitation PDSI Climate change |
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