地球科学进展 ›› 2001, Vol. 16 ›› Issue (6): 836 -841. doi: 10.11867/j.issn.1001-8166.2001.06.0836

研究论文 上一篇    下一篇

三江平原湿地消长与区域气候变化关系研究
张树清;张柏;汪爱华   
  1. 中国科学院长春地理研究所,吉林 长春 130021
  • 收稿日期:2001-05-21 修回日期:2001-08-15 出版日期:2001-12-20
  • 通讯作者: 张树清 E-mail:shqzhang@263.net
  • 基金资助:

    中国科学院创新工程项目“国家资源环境数据库建设与数据共享研究”(KZCX2-308-3)专题之五,及中国科学院湿地过程与环境开放实验室基金资助.

A STUDY ON THE RELATIONSHIP BETWEEN DISTRIBUTIVE VARIATION OF WETLANDS AND REGIONAL CLIMATE CHANGE IN SANJIANG PLAIN

ZHANG Shuqing,  ZHANG Bai,  WANG Aihua   

  1. Changchun Institute of Geography, CAS, Changchun 130021,China
  • Received:2001-05-21 Revised:2001-08-15 Online:2001-12-20 Published:2001-12-01

以遥感手段为主,提取近20年来多个时期三江平原湿地变化动态数据。将湿地动态数据与历年气象数据相对变化比较处理后,再作灰色关联分析,可以发现它们之间的相互关系。研究表明三江平原湿地面积减小迅速,三江平原区域气候环境变化剧烈,超过全球气候变化速度。通过灰色关联分析可以发现,湿地在维持区域"冷湿"效应中作用突出,三江平原湿地的变化与气温变化成负相关,与降水、湿度变化成正相关。湿地消长与气候要素中的降水因子的相关关系最大,与日照因子相关关系较低,与降雪因子几乎无关。

Because of human activities, climate change nowadays essentially differs with that of the past, and the range of climate change in the 100 years has far exceeded that of past 10,000 years. As a most essential factor to control the distributive variation of wetlands, the change of climate greatly influences on material circle, energy flow, the productivity and propagation of wetlands. The relationship between climate change and the distributive variation of wetlands has been attached importance to by human being.Sanjiang plain, where is the biggest fresh wetlands distributed area in China, has been reclaimed for many years and has became a famous base of cash foodstuff. Because of the loss of wetlands, the environment has deteriorated, the temperature has increased, and the humidity has decreased. The pace of climate change in this region exceeds that of global change.From remote sensing data and wetland survey data, the dynamic data of wetlands in Sanjiang plain in last two decades has been acquired. Do unitary process to the dynamic data of wetlands and climate data and make them comparable. Based on these, using gray relevancy analysis we can find out the relationship of them. The results show that wetlands play an important role on balancing the regional cold and wet weather. The variation of wetlands in Sanjiang plain is negatively related with the temperature changes, positively related with the precipitation changes and the humidity changes. The distributive variation of wetlands has the closest relationship with precipitation, has less relationship with sunshine, and has almost nothing to do with snow.

中图分类号: 

 [1]  Houghton R A, Woodwell G M. Global Climate Change[M].Sci Am, 1989.36-44.
 [2] Yan Xiaodong, Zhao Shidong, Fu Congbin, et al. How Should the Xiao Xinggan Mt forests change with potential climate change: a simulation Study[J].Journal of Natural Resourees, 1999,14(4): 372-376.[延晓冬,赵士洞,符淙斌,等.气候背景下小兴安岭天然林的模拟研究[J].自然资源学报,1999,14(4):372-376.]
[3] Cao Mingkui, Li Kerang. Perspective on terrestrial ecosystem elimate interaction[J]. Advance in Earth Science, 2000,15(4): 446-451.[曹明奎,李克让.陆地生态系统与气候相互作用的研究进展[J].地球科学进展,2000,15(4):446-451.]
[4]  Kemp D D. Climate change 1995: The science of climate change—contribution of working Group 1 to the second assessment report of the Intergovermental Panel on Climate Change[J]. Progress in Physical Geography,1997,21(3):309-312.
[5]  Poianik A. climate Change and Northern Prairie wetlands: simulations of long-term Dynamics[J]. Limnology of Oceanography,1996,41(5): 871-881.
[6]  Schmidt R. Late and post-glacial history of meromictic langsee, in respect to climate change and anthropogenic impact[J]. Aquat Science, 1998, 60(1): 56-88.
[7] Ji Zhongchun. A Preliminary study on riverain and lakeside wetland in historical period in China[J].Scientia Geographica Sinica, 1997,17(supp.):464-471.[季中淳.中国历史时期对河湖湿地的认识研究[J].地理科学,1997,17(增刊):464-471.]
[8] Chen Guichen, Peng Min, Li Laixing. Characteristics of wetland environment of Qinghai Lake and its conservation and rational Use[A]. In:Study of Wetlands in China[C]. Changchun: Jilin Science and Technology Press, 1995. 241-246. [陈桂琛,彭敏,李来兴.青海湖湿地环境特征及其保护与合理利用.见:中国湿地研究[C].长春:吉林科学技术出版社,1995.241-246.]
[9] Chen Shupeng, Zhao Yingshi. Geo-science Analyses of Remote Sensing[M]. Beijing: The Publishing House of Surveying and Mapping, 1990.250-251.[陈述彭,赵英时.遥感地学分析[M].北京:测绘出版社,1990.250-251.]
[10] Zhang Zhenke, Wu Ruijin, Wang Sumin. The historical environmental change of the frequency and magnetization of the sediment in Daihai Lake[J]. Geographical Research, 1998,17(3):297-302.[张振克,吴瑞金,王苏民.岱海湖泊沉积物频率、磁化率的历史时期环境变化[J].地理研究,1998,17(3):297-302.]
[11] Shen Dajun, Liu Changming. The impact of the system of hydrology and water resource on climate change[J]. Geographical Research, 1998,17(4):435-441.[沈大军,刘昌明.水文、水资源系统对气候变化的影响[J].地理研究,1998,17(4):435-441.]
[12] Liu Xingtu. Wetland resources and Its sustainable use in Songnen-Sanjiang plain[J]. Scientia Geographica Sinica, 1997,17(supp.):451-460.[刘兴土.松嫩—三江平原湿地资源及其可持续利用[J],地理科学,1997,17(增刊):451-460.]
[13] Guo Daben, Wei Yongxia. The study on land utilization( reclamation) and environmental situation change in Sanjiang plain[J]. Scientia Geographica Sinica, 1997,17(supp.): 473-478.[郭大本,魏永霞.三江平原土地利用(开垦)和环境情势变化研究[J],地理科学,1997,17(增刊):473-478.]
[14] Chen Gangqi, Ma Xuehui. Research on changes of ground feather and water balance of mire before and after mire reclamation in Sanjiang plain[J]. Scientia Geographica Sinica, 1997,17(supp.) 427-433. [陈刚起,马学慧.三江平原沼泽开垦后下垫及水平衡变化研究[J].地理科学,1997,17 (增刊):427-433.]
[15] Deng Julong. Grey System Methods[M]. Wuhan: Huazhong Science and Engineering University Press,1992.21-22.[邓聚龙.灰色系统方法[M].武汉:华中理工大学出版社,1992.21-22.]

[1] 单薪蒙, 温家洪, 王军, 胡恒智. 深度不确定性下的灾害风险稳健决策方法评述[J]. 地球科学进展, 2021, 36(9): 911-921.
[2] 段伟利, 邹珊, 陈亚宁, 李稚, 方功焕. 18792015年巴尔喀什湖水位变化及其主要影响因素分析[J]. 地球科学进展, 2021, 36(9): 950-961.
[3] 王澄海, 张晟宁, 张飞民, 李课臣, 杨凯. 论全球变暖背景下中国西北地区降水增加问题[J]. 地球科学进展, 2021, 36(9): 980-989.
[4] 王慧,张璐,石兴东,李栋梁. 2000年后青藏高原区域气候的一些新变化[J]. 地球科学进展, 2021, 36(8): 785-796.
[5] 田凤云,吴成来,张贺,林朝晖. 基于 CAS-ESM2的青藏高原蒸散发的模拟与预估[J]. 地球科学进展, 2021, 36(8): 797-809.
[6] 马宁. 40年来青藏高原典型高寒草原和湿地蒸散发变化的对比分析[J]. 地球科学进展, 2021, 36(8): 836-848.
[7] 张子洋, 闫明, MULVANEY Robert, 季峻峰, 效存德, 刘雷保, 安春雷. 东南极 LGB69冰芯 17122001年气温变化记录的初步研究[J]. 地球科学进展, 2021, 36(2): 172-184.
[8] 崔林丽, 史军, 杜华强. 植被物候的遥感提取及其影响因素研究进展[J]. 地球科学进展, 2021, 36(1): 9-16.
[9] 龙上敏,刘秦玉,郑小童,程旭华,白学志,高臻. 南大洋海温长期变化研究进展[J]. 地球科学进展, 2020, 35(9): 962-977.
[10] 蔡运龙. 生态问题的社会经济检视[J]. 地球科学进展, 2020, 35(7): 742-749.
[11] 萧凌波. 17361911年华北饥荒的时空分布及其与气候、灾害、收成的关系[J]. 地球科学进展, 2020, 35(5): 478-487.
[12] 熊建国, 李有利, 张培震. 夷平面研究新进展[J]. 地球科学进展, 2020, 35(4): 378-388.
[13] 武登云, 任治坤, 吕红华, 刘金瑞, 哈广浩, 张弛, 朱孟浩. 冲积扇形态与沉积特征及其动力学控制因素:进展与展望[J]. 地球科学进展, 2020, 35(4): 389-403.
[14] 胡利民,石学法,叶君,张钰莹. 北极东西伯利亚陆架沉积有机碳的源汇过程研究进展[J]. 地球科学进展, 2020, 35(10): 1073-1086.
[15] 王亚锋,芦晓明,朱海峰,梁尔源. 高山树线的调查与研究方法[J]. 地球科学进展, 2020, 35(1): 38-51.
阅读次数
全文


摘要