1982-2010年中国草地覆盖度的时空动态及其对气候变化的响应
Spatial-temporal dynamics of grassland coverage and its response to climate change in China during 1982-2010
查看参考文献42篇
文摘
|
基于1982-2006年的GIMMS NDVI 数据和2001-2010年的MODIS NDVI 数据反演中国草地覆盖度的空间格局和变化趋势,结合1982-2010年中国气象站点气温和降水数据,分别从不同时空尺度和不同草地类型上分析中国草地覆盖度的年际和月际变化对气候变化的响应。结果表明:(1) 1982-2010年间中国草地分布区气温呈上升趋势(0.04 oC/年),降水量呈减少趋势(-0.39 mm/年),西北干旱区气候暖湿化趋势明显。(2)中国草地覆盖度空间上呈现东南高西北低的特征,29年间草地覆盖度平均值为34%,坡面草地覆盖度最高为61.4%,荒漠草地覆盖度最低为17.1%。(3) 29年间中国草地覆盖度总体呈现上升趋势,平均为0.17%/年,西北干旱和青藏高原地区草地覆盖度增加趋势明显。坡面草地覆盖度增加趋势最明显,平均值为0.27%/年,平原草地和草甸增加趋势较小,平均值仅为0.11%/年和0.10%/年。总体上,中国草地覆盖度呈极显著增加(46.03%)和显著增加的面积比例(11%)大于极显著减少(4.1%)和显著减少的面积比例(3.24%)。(4)从年际变化上,草地覆盖度与气温和降水量均呈不显著正相关(R = 0.21;R = 0.1);从不同草地类型上,荒漠草地和平原草地覆盖度受降水量影响较大,而高山亚高山草甸、高山亚高山草地、坡面草地和草甸覆盖度与温度相关性较大。(5)从月际变化上,草地覆盖度与当月气温、降水量具有显著的相关性(R = 0.80;R = 0.76),表明水热因子的季节波动对牧草生长的影响更大;并且所有类型植被覆盖度与前一月气温和降水量的相关系数最大,表现出明显的时滞效应。 |
其他语种文摘
|
Global climate warming has led to significant vegetation changes in the past half century. Grassland in China, most of which is sensitive to climatic change and ecologically fragile region, undergoes a process of prominent warming and drying. It is necessary to investigate the response of grassland to the climatic variations (temperature and precipitation) for a better understanding of the accumulated consequence of climate change. Vegetation coverage, as an important indicator for evaluating grassland ecosystem condition, is used to monitor grassland change. GIMMS NDVI from 1982 to 2006 and MODIS NDVI from 2001 to 2010 were adopted and integrated in this study to extract the time series of grassland coverage, and to analyze its spatial pattern and changes. The response of grassland coverage to climatic variations at annual and monthly time scales was analyzed using temperature and precipitation time series at Chinese meteorological stations from 1982 to 2010. During the 29 years, the national annual surface air temperature increased with an annual rate of 0.04oC, while national precipitation decreased with an annual rate of -0.39 mm with the exception of Northwest China. Grassland coverage distribution increased from northwest to southeast across China. During 1982-2010, the mean national grassland coverage was 34% but exhibited apparent spatial heterogeneity being highest (61.4%) in slope grasslands and lowest (17.1%) in desert areas. There was a slight increase of the grassland coverage over the study period with an annual rate of 0.17%. Regionally, the largest increase in the grassland area was observed in Northwest China and Tibetan Plateau. The increase in slope grassland areas was as high as 0.27% per year, while in the plain grassland and meadow, the grassland coverage increase was the lowest (being 0.11% per year and 0.1% per year, respectively). Across China, the grass coverage with extremely significant (P<0.01) and significant (P<0.05) area increases accounted for 46.03% and 11% of the total grassland area, respectively, while those with extremely significant and significant decrease were only 4.1% and 3.24% , respectively. At the annual time scale, there were no significant correlations between grassland coverage and annual temperature and precipitation for the total grassland area. However, the grass coverage was mainly affected by temperature in alpine and sub-alpine grassland, alpine and sub-alpine meadow, slope grassland and meadow, while grass coverage in desert grassland and plain grassland was mainly affected by precipitation. At the monthly time-scale, there are significant correlations between grass coverage with both temperature and precipitation, indicating that the grass coverage is mainly affected by seasonal fluctuations of the hydrothermal factors. Additionally, there is obvious time lag-effect between grass growth and climate factors for each grassland type: the highest correlations are observed between the grass coverage and temperature and precipitation of the preceding month. |
来源
|
地理学报
,2014,69(1):15-30 【核心库】
|
DOI
|
10.11821/dlxb201401002
|
关键词
|
草地覆盖度
;
气温
;
降水
;
时空动态
;
相关性
;
滞后效应
|
地址
|
1.
南京大学生命科学学院, 南京, 210093
2.
南京农业大学动物科技学院, 南京, 210095
|
语种
|
中文 |
文献类型
|
研究性论文 |
ISSN
|
0375-5444 |
学科
|
大气科学(气象学);自然地理学 |
基金
|
国家973计划
;
亚太全球变化研究网络(APN)项目
;
国家自然科学基金项目
;
国家863计划
;
澳大利亚国际发展机构(AusAID)项目
|
文献收藏号
|
CSCD:5049783
|
参考文献 共
42
共3页
|
1.
WaKer B.
IGBP Science No.1: A Synthesis of GCTE and Related Research,1997:1-24
|
CSCD被引
2
次
|
|
|
|
2.
Parmesan C. A globally coherent fingerprint of climate change impacts across natural systems.
Nature,2003,421(6918):37-42
|
CSCD被引
404
次
|
|
|
|
3.
Xin Z B. Spatiotemporal variations of vegetation cover on the Chinese Loess Plateau (1981-2006): Impacts of climate changes and human activities.
Science in China series D: Earth sciences,2008,51(1):67-78
|
CSCD被引
65
次
|
|
|
|
4.
Roerink G J. Assessment of climate impact on vegetation dynamics by using remote sensing.
Physics and Chemistry of the Earth, Parts A/B/C,2003,28(1):103-109
|
CSCD被引
53
次
|
|
|
|
5.
信忠保. 气候变化和人类活动对黄土高原植被覆盖变化的影响.
中国科学:D辑,2007,37(11):1504-1514
|
CSCD被引
250
次
|
|
|
|
6.
甘春英. 连江流域近18年来植被覆盖度变化分析.
地理科学,2011,31(8):1019-1024
|
CSCD被引
114
次
|
|
|
|
7.
Keeling C D. Increased activity of northern vegetation inferred from atmospheric CO_2 measurements.
Nature,1996,382(6587):146-149
|
CSCD被引
115
次
|
|
|
|
8.
Weltzin J F. Assessing the response of terrestrial ecosystems to potential changes in precipitation.
Bioscience,2003,53(10):941-952
|
CSCD被引
131
次
|
|
|
|
9.
Hall F G. Satellite remote sensing of surface energy balance: Success, failures, and unresolved issues in FIFE.
Journal of Geophysical Research: Atmospheres (1984-2012),1992,97(D17):19061-19089
|
CSCD被引
17
次
|
|
|
|
10.
Li Z T. Interannual variability of vegetation in the United States and its relation to El Nino/Southern Oscillation.
Remote Sensing of Environment,2000,71(3):239-247
|
CSCD被引
16
次
|
|
|
|
11.
Zhou L M. Variations in northern vegetation activity inferred from satellite data of vegetation index during 1981 to 1999.
Journal of Geophysical Research: Atmospheres (1984-2012),2001,106(D17):20069-20083
|
CSCD被引
157
次
|
|
|
|
12.
Myneni R B. Increased plant growth in the northern high latitudes from 1981 to 1991.
Nature,1997,386(6626):698-702
|
CSCD被引
374
次
|
|
|
|
13.
方精云. 近20年来中国植被活动在增强.
中国科学C辑,2003,33(6):554-565
|
CSCD被引
209
次
|
|
|
|
14.
李霞. 气候变化对中国北方温带草原植被的影响.
北京师范大学学报:自然科学版,2006,42(6):618-623
|
CSCD被引
41
次
|
|
|
|
15.
朴世龙. 最近18年来中国植被覆盖的动态变化.
第四纪研究,2001,21(4):294-302
|
CSCD被引
171
次
|
|
|
|
16.
Zhang J. Seasonal characters of regional vegetation activity in response to climate change in West China in recent 20 years.
Journal of Geographical Sciences,2006,16(1):78-86
|
CSCD被引
11
次
|
|
|
|
17.
赵茂盛. 应用遥感数据研究中国植被生态系统与气候的关系.
地理学报,2001,56(3):287-296
|
CSCD被引
74
次
|
|
|
|
18.
孙艳玲. 内蒙古植被覆盖变化及其与气候、人类活动的关系.
自然资源学报,2010,25(3):407-414
|
CSCD被引
99
次
|
|
|
|
19.
Sun J. On the variation of NDVI with the principal climatic elements in the Tibetan Plateau.
Remote Sensing,2013,5(4):1894-1911
|
CSCD被引
39
次
|
|
|
|
20.
吴瑞芬. 内蒙古典型草本植物春季物候变化及其对气候变暖的响应.
生态学杂志,2009,28(8):1470-1475
|
CSCD被引
23
次
|
|
|
|
|