全球变化研究

陆地表层水贮量变化对海平面上升贡献的综合评估

展开
  • 中国科学院寒区旱区环境与工程研究所,甘肃 兰州  730000
丁永建(1958-),男,甘肃天水人,研究员,主要从事寒区水文与环境研究. E-mail:dyj@ns.lzb.ac.cn

收稿日期: 2000-03-15

  修回日期: 2000-07-10

  网络出版日期: 2001-02-01

基金资助

中国科学院冰冻圈动态变化基础研究(三期)和国家自然科学基金项目“青藏高原典型地区多年冻土活动层内水文过程模拟研究”(编号:49971022)联合资助.

ASSESSMENT ON CONTRIBUTIONS OF LAND WATER STORAGE TO SEA LEVEL RISE

Expand
  • Cold and Arid Regions Environmental and Engineering Research Institute,CAS,Lanzhou730000,China

Received date: 2000-03-15

  Revised date: 2000-07-10

  Online published: 2001-02-01

摘要

由于气候变暖和人为活动的加剧,大陆表面水贮量正在发生着显著的变化,这必将引起海平面的变化。然而,陆地表层水贮量的变化是非常复杂的。主要讨论了地下水、人工水库、天然湖泊和森林退化对海平面影响的主要研究结果,重新评估了这些因素对海平面贡献的程度,尤其是考虑了中国相关因子的作用。还就一些很不确定的因素,如水库深层渗透水、土壤水贮量变化、灌溉蒸腾等对海平面的影响也进行了初步讨论。

本文引用格式

丁永建,秦大河,叶柏生,刘时银 . 陆地表层水贮量变化对海平面上升贡献的综合评估[J]. 地球科学进展, 2001 , 16(1) : 106 -112 . DOI: 10.11867/j.issn.1001-8166.2001.01.0106

Abstract

The surface water and ground water storages are changing due to direct anthropogenic and climatic causes. Changes of the surface water and ground water storage should arouse sea level rise. However, changes of the surface water and ground water storage are very complicated. Their effect on the sea level is attributed by the ground water depletion, changes in man made reservoir and natural lake storage, deforestation, loss of wetlands, permafrost thawing, retreating of glaciers and ice sheets and increase in soil moisture and so on. This paper focuses on effect of the ground water, man made reservoir, natural lake and deforestation on the sea level. We re examine recent estimates and re assess the contributions of those factors to sea level rise, especially added the contributions of some corresponding factors from China, which have been neglected in former studied. Some overestimates and uncertain factors such as deep seepage beneath reservoirs, evaporation over reservoirs,soil water storage, evaporation and transpiration by irrigation are discussed. The contribution of the total excess charge for the global ground water to the sea level rise might fall in the range of 0.35~0.45 mm/a, and the cumulating sea level rise caused by this factor is estimated to be 11.05 mm. We suggest that the total water impoundment at present would be about 5.0×1012 ~6.0×1012 m3 (by 50% to 60% of total reservoir capacity) in the world. These figures amount to a 13.9 to 16.7 mm sea level decrease, equivalent to an average rate of 0.232 to 0.278 mm/a over the last 60 years. The contribution of lake storage to sea level rise estimated is 0.112 mm/a for rate and 3.69 mm for total. The deforested rate of 10×10 10 m2/a is available value to estimate contribution of deforestation to sea level rise in the past 50 years. It would add 3.3×1010 m3/a water to the ocean, amounting to 0.092 mm/a, or 4.58 mm in 50 years.

参考文献

[1]  Gornitz V. Monitoring sea level changes[J]. Climatic Change, 1995,31:515~544.
[2]  Sahagian D L, Jacobs D K, Schwartz F W. Man-made lakes and sea level rise[J]. Nature, 1994,370:258.
[3]  IPCC. Change in Sea level[R]. 1996.379~380.
[4]  Liu Changming,He Xiwu.General Plan on Water Problems in 21st Century in China[M].Beijing:Science Press,1996.[刘昌明,何希吾.中国21世纪水问题方略[M].北京:科学出版社,1996.]
[5]  Liu Changming,He Xiwu,Ren Hongzun.Research on Water Problems in China [M]. Beijing: Meteorological Publishing Press,1996.[刘昌明,何希吾,任鸿遵.中国水问题研究[M].北京:气象出版社,1996.]
[6]  Hou Tongde.Pre-study on Marketable Scheme of Water Resource from the Yellow River[J].Chinese Water Conservancy.[后同德.引黄供水资源市场配置初探[J].中国水利,1993, 2: 9~11.]
[7]  Wenren Xuexing.Analysis on Potential and Status of Groundwater Development in North China[J].Groundwater,1991,13(2):75~78.[闻人雪星.华北地下水资源开发利用现状及潜力分析[J].地下水,1991, 13(2):75~78.]
[8]  Chao B F. Man-made lakes and sea level rise[J]. Nature,1994, 370:258.
[9]  Rodenburg E. Man-made lakes and sea level rise[J]. Nature,1994, 370: 258.
[10]  Avakian A B. Reservoirs of the world and their environmental impact[A]. In: the Impact of Large Water Projects on the Environment. Proceedings of UNESCO/UNEP[C]. Paris: Int Symp,1990. 29~36.
[11]  ICOLD (International Commission on Large Dams). World Dam Register 1988[R]. 1988. 1~25.
[12]  Veltrop J. Benefits of Dams to Society[Z]. USCOLD Newsletter, 1995.
[13]  Takeuchi K. Least marginal environmental impact rule for reservoir development[J]. Hydrological Sciences Journal, 1997, 42(4): 583~597.
[14]  UNESCO. World Water Balance and Water Resources of the Earth[R]. Studies and Reports in Hydrology 25, USSR National Committee for IHD, UNESCO,1978.
[15]  Kundzewicz Z W. Water resources for sustainable development[J]. Hydrological Sciences Journal, 1997, 42(4): 467~480.
[16]  Qin B Q, Huang Q. Evaluation of the climatic change impacts on the inland lake—a case study of Lake Qinghai, China[J]. Climatic Change, 1998, 39: 695~714.
[17]  Couzin J. Landscape changes make regional climate run hot and cold[J]. Science, 1999, 283: 317.
[18]  Shi Yafeng,Zhou Kejun.Characteristics,Change in the near Future and Environmental Effects of Surface Water in China[A]. In: Ye Duzheng, Chen Panqunet al. Pre-research onGlobal Change in China[C].Beijing:Seismological PublishingPress,1992,85~158.[施雅风,周克俊.中国地表水体特征、近期变化及其对环境的影响[A].见:叶笃正,陈泮勤主编.中国的全球变化预研究[C].北京:地震出版社,1992. 85~158.]
[19]  Ding Yongjian,Liu Fengjing.Trend Forecast on the effect of Climatic Change in the Last 30 years to the Elements of Water Balance in the Qinghai Lake Basin[J].Scientia Geographica sinica,1993,15(2):128~135.[丁永建,刘风景.近30年来青海湖流域气候变化对水量平衡要素的影响及其趋势预测[J].地理科学,1993, 15(2):128~135.]
[20]  Liu Changming,Zhong Junxiang.Pre-analysis on the Effects of the Forest to the Runoff in the Loess Plateau[C].Acta Geographical Sinica,1978,33(2):112~127.[刘昌明,钟骏襄.黄土高原森林对年径流影响的初步分析[J].地理学报,1978, 33(2): 112~127.]
[21]  Henderson-Sellers A, Dickinson R E, Durbridge T B,et al.Tropical deforestation: modeling local-to regional-scale climate change[J]. J Geophys Res, 1993, 98: 7 289~7 315.
[22]  Bawa K S, Dayanandan S. Socioeconomic factors and tropical deforestation[J]. Nature, 1997, 386: 562~563.
[23]  Skole D, Tucker C. Tropical deforestation and habitat fragmentation in the Amazon: satellite data from 1978 to 1988[J]. Science, 1993, 260: 1 905~1 910.
[24]  Smith T J. Imperilled wetlands[J]. Nature, 1998, 395: 131~132.
[25]  Soul M E, Sanjayan M A. Conservation targets: do they help? [J]. Science, 1998, 279: 2 060~2 061.
[26]  Houghton R A. The worldwide extent of land-use change[J]. BioScience, 1994, 44(5): 305~313.
[27]  FAO/UNEP. Tropical Forest Resources Assessment Project[R]. FAO, Rome. 1981.
[28]  Cood and Agriculture Organization of the United Nations (FAO). Forest Resources Assessment 1990 Program: Tropical Countries[R]. FAO Forestry Paper 112, Rome. 1993.
[29]  Ren Hongzun.Analysis on the Problems of Water Shortage in China[A].In:Liu Changming,He Xiwu,Ren Hongzun.Research on Water Problems in China[C].Beijing:Meteorological Publishing Press,1996,13~18.[任鸿遵.我国缺水问题分析[A].见:刘昌明,等编.中国水问题研究[C].北京:气象出版社,1996. 13~18.]
[30]  Golubev G N. Economic activity, water resources and environment: a challenge for hydrology[J]. Hydrological Sciences Journal, 1983, 28(1): 57~75.
[31]  Shiklomanov I A. Irrigation and River Runoff in Russian[M]. Vodnye Resursy, N5, 1976. 14~25.
[32]  Lin Xingcui.Suggests on Developing the Water-saving Irrigated Agriculture in the Arid Region North of China[J].AridRegion Arricultural Research,1994,12(1):79~83.[林性粹.我国北方旱区发展节水灌溉农业雏议[J].干旱地区农业研究,1994, 12(1): 79~83.]

Options
文章导航

/