地理学报 ›› 2011, Vol. 66 ›› Issue (3): 385-395.doi: 10.11821/xb201103011
张淑兰1, 于澎涛1, 王彦辉1, 张海军2, Valentina Krysanova3, HUANG Shaochun3, 熊伟1, 徐丽宏1
收稿日期:
2010-11-15
修回日期:
2010-12-21
出版日期:
2011-03-20
发布日期:
2011-03-20
通讯作者:
于澎涛(1970-), 女, (蒙古族), 内蒙古自治区开鲁县人, 副研究员, 博士, 中国地理学会会员(S110004402M), 主要从事森林水文及模型应用研究。E-mail: yupt@caf.ac.cn
作者简介:
张淑兰(1980-), 女, 河北省滦南县人, 博士生, 主要从事森林生态、水文与水资源管理研究。E-mail: zhangshulan1980@163.com
基金资助:
国家自然科学基金项目(40730631; 41071023); 林业公益性行业科研专项经费项目(200904056; 200904005);中国林科院中央级公益性科研院所基本科研业务费专项资金项目(CAFYBB2007038; CAFYBB2010001-02);国家林业局六盘山森林定位站和森林生态环境重点开放性实验室资助
ZHANG Shulan1, YU Pengtao1, WANG Yanhui1, ZHANG Haijun2, Valentina Krysanova3, HUANG Shaochun3, XIONGWei1, XU Lihong1
Received:
2010-11-15
Revised:
2010-12-21
Online:
2011-03-20
Published:
2011-03-20
Supported by:
National Natural Science Foundation, No.40730631; No.41071023; Forestry Industry Research Special Funds for Public Welfare Projects, No.200904056; No.200904005; Special Funds Projects for Basic Scientific Research Business Expenses of Central Public Welfare Research Institutes in Chinese Academy of Forestry, No.CAFYBB2007038; No. CAFYBB2010001-02; The Forest Orientation Station for Liupan Mountain State of Forestry Administration and Forest Ecological Environment Key Open Lab Funding
摘要: 利用分布式生态水文模型SWIM,基于泾河上游(泾川测站以上) 植被、土壤、气象和水文数据对研究区进行了水文过程的模拟,从而估算了流域的实际蒸散量及其各组分。结果表明:SWIM模型能够较好的模拟泾河上游流域的水文过程,模拟的流域多年(1997-2003 年) 平均实际蒸散量为443 mm,其中土壤蒸发量为259 mm,植被蒸腾量为157 mm,冠层截持量为27 mm。石质山区的森林覆盖区和非森林地的年蒸散总量在整个流域分别具有最大值和最小值,为484 mm和418 mm;黄土区实际蒸散量介于二者之间,平均为447 mm。森林覆盖地区土壤蒸发明显小于其它区域,而蒸腾和冠层截留明显大于其它区域。年内蒸散量主要集中在5-8 月份,占全年总蒸散量的60%,且冠层蒸散比例较大达63%。整个流域湿润年份较干旱年份蒸散量增加了78 mm,其中土壤蒸发增加最多,其次是冠层蒸腾,冠层截留蒸发最小。
张淑兰, 于澎涛, 王彦辉, 张海军, Valentina Krysanova, HUANG Shaochun, 熊伟, 徐丽宏. 泾河上游流域实际蒸散量及其各组分的估算[J]. 地理学报, 2011, 66(3): 385-395.
ZHANG Shulan, YU Pengtao, WANG Yanhui, ZHANG Haijun, Valentina Krysanova, HUANG Shaochun, XIONGWei, XU Lihong. Estimation of Actual Evapotranspiration and Its Component in the Upstream of Jinghe Basin[J]. Acta Geographica Sinica, 2011, 66(3): 385-395.
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