湿地是地球上最为重要而独特的生态系统类型,在缓解全球气候变化和调节区域气候特征方面具有重要作用。以北京湿地为研究案例,在分析湿地气候调节作用过程机理的基础上,综合运用遥感数据和常规气象站点监测资料,利用CASA模型和植被指数累积模型分别定量反演获得北京湿地年地上生物量和年蒸散量,基于价值量方法定量评估了北京城市湿地气候调节能力。结果表明:①北京湿地地上生物量吸收固定二氧化碳和释放氧气分别约为1.42×108kg和1.03×108kg,价值量分别约为2.83亿元和0.42亿元;②北京湿地蒸散发量约为4.16亿m3,价值量约为1.14亿元。③北京湿地通过固碳释氧和地表蒸散发等过程所形成的气候调节功能总价值约为4.39亿元。
杨一鹏
,
曹广真
,
侯鹏
,
蒋卫国
,
陈云浩
,
李京
. 城市湿地气候调节功能遥感监测评估[J]. 地理研究, 2013
, 32(1)
: 73
-80
.
DOI: 10.11821/yj2013010008
Wetland is one of the most important and extraordinary ecosystems.It plays a key role in decelerating the climatic change trend and regulating the regional climatic feature, which is closely related to the human well-being.Based on the satellite images and meteorological data of ground observation stations,Beijing taken as the study region, biological mass and evapotranspiration intensity of wetlands are respectively estimated with CASA(Carnegie-Ames-Stanford Approach)model and NDVI(Normal Difference Vegetation Index)cumulative model,then regulation valuation implemented by carbon sequestration, oxygen release and evapotranspiration are evaluated with carbon tax method,shadow project method and results reference method.The results show that:(1)The quality of carbon dioxide sequestration and oxygen release by wetlands in Beijing is about 1.42×108 kg and 1.03×108 kg respectively,which are about 283 million yuan and 42 million yuan in turns in 2007.(2) The capacity of water vapor evapotranspired from wetlands is about 416 million m3,which is about 114 million yuan in 2007.In general,the total valuation of climatic regulation of wetlands is about 439 million yuan in 2007.
[1] 湿地国际.关于特别是作为水禽栖息地的国际重要湿地公约.http://www.wetwonder.org,1982-3-12.
[2] 联合国环境与发展大会.联合国气候变化框架公约.http://unfccc.int,1992-5-9.
[3] 陈克林,张小红,吕咏.气候变化与湿地.湿地科学,2003,1(1):73-77.
[4] Urban and Regional Carbon Management.What is urban and regional carbon management?http://www.gcp-urcm.org, 2012-2-24.
[5] Potter C S,Randerson J T,Field C B,et al.Terrestrial cosystem production:A process model based on global satellite and surface data.Global Biogeochemical Cycle,1993,7(4):811-841.
[6] 孙睿,刘昌明,李小文.利用累积NDVI估算黄河流域年蒸散量.自然资源学报,2003,18(2):155-161.
[7] Myneni R B,Knyazikhin Y,Zhang Y,et al.MODIS leaf area index(LAI)and fraction of photosynthetically active radiation absorbed by vegetation(FPAR)product(MOD15)Algorithm Theoretical Basis Document.http://eospso.gsfc. nasa.gov/atbd/modistables.Html,1999-4-30.
[8] 李刚,辛晓平,王道龙,等.改进CASA模型在内蒙古草地生产力估算中的应用.生态学杂志,2007,26(12): 2100-2106.
[9] 周广胜,张新时.自然植被净第一性生产力模型初探.植物生态学报,1995,19(3):193-200.
[10] Donald O R,Thomas C W,Donald C B et al.Comparison of 15 evaporation methods applied to a small mountain lake in the northeastern USA.Journal of Hydrology,2007,340:149-166.
[11] Robert C,Ralph A,Rudolf G et al.The value of the world's ecosystem services and natural capital.Nature,1997,387: 253-260.
[12] 王继国.湿地调节气候生态服务价值的估算——以新疆艾比湖湿地为例.江苏技术师范学院学报,2007,13(4): 58-62.
[13] 周葆华,操璟璟,朱超平,等.安庆沿江湖泊湿地生态系统服务功能价值评估.地理研究,2011,30(12):2296-2304.