生态与农村环境学报 ›› 2016, Vol. 32 ›› Issue (2): 243-251.doi: 10.11934/j.issn.1673-4831.2016.02.012

• 区域环境与发展 • 上一篇    下一篇

近30 a雅鲁藏布江流域高寒湿地动态变化及其对气候变化的响应

刘冬1, 王涛2, 沈渭寿1, 林乃峰1, 邹长新1   

  1. 1. 环境保护部南京环境科学研究所, 江苏南京 210042;
    2. 南京信息工程大学地理与遥感学院, 江苏南京 210044
  • 收稿日期:2015-03-26 出版日期:2016-03-25 发布日期:2016-04-01
  • 通讯作者: 邹长新,E-mail:zcx@nies.org E-mail:zcx@nies.org
  • 作者简介:刘冬(1984-),女,河南洛阳人,助理研究员,博士,主要从事气候变化与生态安全方面的研究。E-mail:liudong@nies.org
  • 基金资助:

    国家"十二五"科技支撑计划(2012BAC19B06-1);国家自然科学基金青年基金(41501596);江苏省普通高校研究生科研创新计划(KYLX15_0869)

Dynamic of the Alpine Wetlands and Its Response to Climate Change in the Yarlung Zangbo River Valley in Recent 30 years

LIU Dong1, WANG Tao2, SHEN Wei-shou1, LIN Nai-feng1, ZOU Chang-xin1   

  1. 1. Nanjing Institute of Environmental Sciences, Ministry of Environmental Protection, Nanjing 210042, China;
    2. School of Geography and Remote Sensing, Nanjing Universitos of Information Science & Technology, Nanjing 210044, China
  • Received:2015-03-26 Online:2016-03-25 Published:2016-04-01

摘要:

利用1980、1990、2000和2010年4期Landsat、环境一号卫星遥感影像提取雅鲁藏布江(以下简称"雅江")流域湿地面积动态变化信息,并结合实地调查和近30 a气象、水文、积雪数据研究湿地动态变化对气候变化的响应特征。结果表明,2010年雅江流域高寒湿地面积占流域总面积的3.73%,其中以沼泽湿地面积最大(59.46%),其次为河流(30.19%)、湖泊(10.13%)和人工湿地(0.23%);近30 a间雅江流域湖泊湿地和河流湿地面积总体上呈增加趋势,而沼泽湿地面积呈降低趋势;近30 a来雅江流域年均温、年均最高温和年均最低温均呈显著增加趋势,降水量波动较大,呈轻微增加趋势但不显著,平均相对湿度呈不显著下降趋势。年均气温和年均最高气温这2个因素与雅江流域湖泊面积变化相关性显著,河流湿地面积、雅江5大支流干流河长的增长分别与年均温、年均最高温、年均最低温相关性显著,沼泽湿地面积与该区域气温以及平均相对湿度相关性显著,开发大坝、水库等国家建设战略是雅江流域人工湿地面积增加的主要驱动力。

关键词: 高寒湿地, 雅鲁藏布江, 气候, 响应

Abstract:

The knowledge about dynamic of the alpine wetlands in the Yarlung Zangbo River Valley and its response to climate change would help understand in depth variation of the alpine ecosystem of the Qinghai Tibet Plateau and its response to global climate change. Information dynamics of the wetlands, in area, in the Yarlung Zangbo River Valley was extracted from the remote sensing images and data transmitted from the Landsat and Environmental Satellite #1 in 1980, 1990, 2000 and 2010, and collated with the data obtained in field surveys and the recent 30 years of metereological, hydrological and snow-accumulation data to explore dynamics of wetlands and its response to climate change. Results show that in 2010 alpine wetlands accounted for 3.73% of the whole valley in area, with swampy wetlands being the largest in area and accounting for 59.46% of the total area of the wetlands, followed by riverine wetlands (30.19%), lacustrine wetlands (10.13%) and man-made wetlands (0.23%). In the recent 30 years riverine and lacustrine wetlands have been on a rising trend in area, while swampy wetlands on a reverse trend. The Yarlung Zangbo River Valley has been on a rising trend in annual mean temperature, mean annual maximum temperature, and mean annual minimum temperature, fluctuating greatly or on a slightly, but not apparently, rising trend in precipitation, and a declining trend, though not apparent, in mean relatively humidity. The changes in annual mean temperature and mean annual maximum temperature were significantly related to the changes in the area of the lakes in the valley; the increases in the area of the riverine wetlands and in the length of the main streams of the five major tributaries of the Yarlung Zangbo River were to the changes in annual mean temperature, mean annual maximum temperature, and mean annual minimum temperature; and the area of the swampy wetlands was to the air temperature and annual mean relative humidity. The country's strategy of construction, like building dams and reservoirs is the major driving force of the increase in the area of man-made wetlands in the river valley.

Key words: alpine wetland, Yarlung Zangbo River, climate, response

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