globalchange  > 气候变化事实与影响
CSCD记录号: CSCD:6379731
论文题名:
扎龙湿地土地利用/覆盖类型时空演变及其气候响应
其他题名: Spatiotemporal Evolution of Land Cover Types and Response to Climate Change in Zhalong Wetland
作者: 于成龙1; 刘丹1
刊名: 生态环境学报
ISSN: 1674-5906
出版年: 2018
卷: 27, 期:11, 页码:2117-2126
语种: 中文
中文关键词: 土地利用/覆盖 ; 时空演变 ; 气候响应 ; 扎龙湿地
英文关键词: land use/cover ; spatiotemporal evolution ; climate response ; Zhalong Wetland
WOS学科分类: ENVIRONMENTAL SCIENCES
WOS研究方向: Environmental Sciences & Ecology
中文摘要: 基于Landsat和HJ星数据,采用决策树、面向对象分类、GIS空间分析、线性拟合、相关分析等方法研究了20002017年扎龙湿地土地利用/覆盖时空格局变化及其对气候因子的响应,为湿地生态气象综合监测评估提供数据及方法支撑。结果表明,(1)草甸一直是扎龙湿地的主要土地利用/覆盖类型,面积在1326.70~1513.87 km~2之间变化,平均占该湿地总土地面积的65.15%,2001年以来面积以7.21 km~2·a~(-1)的速度显著下降。核心区90%以上为草甸,缓冲区和试验区的草甸所占比例依次降低,不同类型的草甸年际间相互转换频繁,总体上呈现此消彼长的现象。(2)农田面积在281.80~364.65 km~2之间变化,平均占总土地面积的14.24%,以4.15 km~2·a~(-1)的速度呈极显著上升趋势,绝大多数农田分布在试验区内。(3)水体和农田的地理中心有明显向东北方向转移的趋势,其他土地利用/覆盖类型的地理中心虽然在部分年份有较大波动,但总体上未见有明显聚集或转移趋势。(4)气象因子年际变化幅度小将更有利于扎龙湿地明水体和草甸的维持和发展,有地表水覆盖的草甸景观格局变化的主要驱动因子为温度,无地表水草甸变化的主要驱动因子为水分。
英文摘要: Zhalong Wetland, which is located in poor meteorological conditions, sensitive area of the global change, and fragile ecological environment, has a poor health in recent decades. Based on data of Landsat and HJ, we took Zhalong Wetland as an example and tried to identify change of land use/cover patterns and its climate response mechanism from 2000 to 2017 by using decision tree method, object-oriented classification, GIS spatial analysis, linear fitting method, correlation analysis and so on. This paper would provide data and methods for wetland comprehensive monitoring and evaluation of ecologic meteorology. The results were as followed. Marshland was the main land cover type in Zhalong Wetland. Its area varied from 1326.70 to 1513.87 km~2 and accounted for 66.17% of the whole wetland on average and had decreased significantly at the rate of 7.21 km~2·a~(-1) since 2001. More than 90% of core area was marshland, and the proportion of marshland in buffer area and experimental area was reduced in turn. The interannual conversion among different types of marshlands was frequent in general. Farmland area varied from 281.80 to 364.65 km~2 and accounted for 16.42% of the whole wetland. It showed a significant increasing trend at the rate of 4.15 km~2·a~(-1), and most of that was distributed in the experimental area. Both the geographic centers of water body and farmland had the tendency of moving toward northeast. The geographic centers of the other land types fluctuated considerably in some years, but there was no obvious trend of aggregation or transfer on the whole. The small interannual fluctuation of meteorological factors would be more favorable to the maintenance and development of water and marshland. Temperature was the main driving factor of the change of landscape pattern in marshland with surface water, and water was the main driving factor in marshland without surface water.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/157629
Appears in Collections:气候变化事实与影响

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作者单位: 1.中国气象局东北地区生态气象创新开放实验室
2.黑龙江省气象院士工作站
3.黑龙江省气象科学研究所, 中国气象局东北地区生态气象创新开放实验室
4., 哈尔滨
5.哈尔滨
6.哈尔滨, 黑龙江
7.黑龙江
8.黑龙江 150030
9.150030
10.150030, 中国

Recommended Citation:
于成龙,刘丹. 扎龙湿地土地利用/覆盖类型时空演变及其气候响应[J]. 生态环境学报,2018-01-01,27(11):2117-2126
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