The Response Relation between Climate Change and NDVI over the Qinghai-Tibet plateau
Based on a long-term vegetation index dataset of NDVI and meteorological data from 68 meteorological stations in the Qinghai-Tibet plateau and their relations with major climate factors were analyzed. The results show the following: 1) The linear trends of temperature in the Qinghai-Tibet plateau indicate that the temperature in the plateau generally increased, but it rose faster in the last 20 years. 2) The most significant NDVI increase occurred in the eastern and southern plateau. However, the western and northern plateau demonstrate a decreasing trend. 3) There is a significant positive linear correlation between NDVI and temperature and a negative correlation between NDVI and mean wind speed. However, no significant statistical relationship was found between NDVI and relative humidity, precipitation or sunshine duration.4) The changes in NDVI for the plateau are driven by temperature-precipitation, but for the desert and forest areas, the relation changes to precipitation-temperature-wind velocity and wind velocity-temperature-precipitation.
[1] Mo Hang-up, Zhang Bai-ping, Cheng Wei-ming, et al. Major environmental effects of the Tibetan plateau, Progress in Geography,
2004, vol. 23, No. 2, pp. 88-96.
[2] WANG Jing-sheng, ZHANG Xian-zhou, ZHAO Yu-ping, et al. Spatio-temporal pattern of climate changes in Northern Tibet-s Qiangtang
Plateau. Resources science, 2008, vol. 30, No. 12, pp. 1852-1859.
[3] WANG Nan, LI Dong-liang, ZHANG Jie. Research Advance of Surface
Temperature Change over Tibetan Plateau. Journal of Arid Meteorology,
2010, vol. 28, No. 3, pp. 265-269.
[4] Cramer W P,Leemans R. Assessing impacts of climate change vegetation
using climate classification system. In:Solomon A M, Shuart H H(eds.).
Vegetation Dynamics and Global Change, London: Chapman and Hall,
1993, pp. 190-217.
[5] ZHANG Yue-cong, ZHAO Zhi-qiang, LI Shuang-cheng. Indicating
variation of surface vegetation cover using SPOT NDVI in the northern
part of North China. Geographical Research,2008, vol. 27, No. 4, pp. 745-754.
[6] Pettorelli N, Vik J, Mysterud A, et al. Using the satellite derived NDVI to
assess ecological responses to environmental change. Trends in Ecology
& Evolution, 2005, vol. 20, No. 9, pp. 503-510.
[7] Ichii K, Kawabata A, Yamaguchi Y. Global correlation analysis for
NDVI and climatic variables and NDVI trends: 1982-1990 [J]. International Journal of Remote Sensing, 2002, vol. 23, No. 18, pp.
3873-3878.
[8] Piao S, Mohammat A, Fang J, et al. NDVI-based increase in growth of
temperate grasslands and its responses to climate changes in
China.Global Environmental Change,2006, vol. 16, No. 4, pp. 340-348.
[9] Ding M J, Zhang Y L, Liu L S, et al. The relationship between NDVI and
precipitation on the Tibetan Plateau. Journal of Geographical Sciences,
2007, vol. 17, No.3, pp. 259-268.
[10] Tucker C J, Pinzon J E, Brown M E, et al. An Extended AVHRR 8 km
NDVI data set compatible with MODIS and SPOT vegetation NDVI data.
Int. J. Remote Sensing, 2005, vol. 26, No. 20, pp. 4485-4498.
[11] LI Ben-gang, TAO Shu. Correlation between AVHRR NDVI and climate
factors. Acta Ecologica Sinica, 2000, vol. 20, No. 5, pp. 898~902.
[12] LI Xia, LI Xiao-bing, CHEN Yun-hao, et al. Temporal responses of
vegetation to climate variables in temperate steppe of northern China.
Journal of Plant Ecology, 2007, vol. 31, No. 6, pp. 1054-1062.
[13] Gao Z Q, Dennis O. The temporal and spatial relationship between NDVI
and climatological parameters in Colorado. Journal of Geographical
Sciences, 2001, vol. 11, No. 4, pp. 411-419.
[14] CHU Duo,DEJI Yang-zong,PUBU Ciren,et al. The response of typical
vegetation growth to climate conditions in North Tibetan Plateau. Journal
of applied meteorological science, 2007, vol. 18, No. 6, pp. 832-839.
[15] ZHAO Yu-ping, ZHANG Xian-zhou, WANG Jing-sheng, SHEN
Zhen-xi. Correlation Analysis between NDVI and Climatic Factors of
Grassland Ecosystems in the Northern Tibetan Plateau from 1982 to
2003. Resources Science, 2009, vol. 31, No. 11, pp. 1988-1998.
[16] DING Ming-jun, ZHANG Yi-li, LIU Lin-shan, WANG Zhao-feng,
YANG Xu-chao. Seasonal Time Lag Response of NDVI to Temperature
and Precipitation Change and Its Spatial Characteristics in Tibetan
Plateau, Progress in geography, 2010, vol. 29, No.4, pp. 507-512.
[17] MAO Fei, LU Zhi-guang, ZHANG Jia-hua, et al. Relations between
AVHRR NDVI and climate factors in Northern Tibet in recent 20 years.
Acta Ecolgica Sinica, 2007, vol. 27, No.8, pp. 3198-3205.
[18] Zheng Du. Study on natural geographical system of the Qinghai-Tibet
Plateau. Science in China (Series D), 1996, vol. 26, No. 4, pp. 336-341.
[19] LIA NG Si-hai, CHEN Jiang, JIN Xiao-mei, W AN Li, GONG Bin.
Regularity of Vegetation Coverage Changes in the Tibetan Plateau over
the Last 21 Years. Advance in earth science, 2007, vol. 22, No. 1, pp.
33-40.
[20] ZHANG Yi-li, LI Bing-yuan, ZHENG Du. A discussion on the boundary
and area of the Tibetan Plateau in China. Geographical Research, 2002,
vol. 21, No. 1, pp. 1-8.
[21] WEI F Y. Statistic diagnose and foreshadow technology in present
climate. Beijing: Meteorological Press, 1999, pp. 62-79.
[22] XU Z X,TAKEUCHI K,ISHIDAIRA H. Long—term trends of annual
temperature and precipitation time series in Japan. Journal of
Hydroscienee and Hydraulic Engineering, 2002, vol. 20, No. 2, pp. 11-26.
[23] ERCAN K,SERDAR K. Trend analysis of stream flow in Turkey. Journal
of Hydrology, 2004, vol. 289, pp. 128-144.
[24] JIANG Tong, SU Buda, WANG Yanjun, et al. Trends of Temperature,
Precipitation and Runoff in the Yangtze River Basin from 1961 to 2000.
Advances in Climate Change Research, 2005, vol.1, No. 2, pp. 65-68.
[25] Chen Yanli, Long Bu-ju, Pan Xue-biao, Mo Weihua. Grassland
Vegetation Change Based on MODIS NDVI Data and Climate
Information. Journal of Applied Meteorological Science, 2010, vol. 12,
No. 2, pp. 229-236.
[26] IPCC. Climate Change 2001: Impacts, adaptation, and vulnerability.
Summary for Policymakers. A Report of Working Group Ⅱ of the
Intergovernmental Panel on Climate Change. Geneva. Switzerland, 2001.
[27] IPCC. IPCC Fourth Assessment Report(AR4）,Cambridge: Cambridge
University Press, 2007.
[28] LIN Xue-chun, YU Shu-qiu, TANG Guo-li. Series of average air
temperature over China for the last 100-year period. Scientia
atmospherica sinica, 1995, vol. 19, No. 5, pp. 525-534.
[29] QIN Da-he. Colligate Report of Assessment in Environment Evolvement
of West at China. Beijing: Science Press, 2002, pp. 2-10.
[30] MA Xiao-bo, HU Ze-yong. Precipitation Variation Characteristics and
Abrupt Change over Qinhai-Xizang Plateau in Recent 40 Years. Journal
of Desert Research, 2005, vol. 25, No. 1, pp. 137-139.
[31] Yao Li, Wu Qing-mei. Climatic change of characteristics over
Qinghai-Xizang Plateau. Meteorological Science and Technology, 2002,
vol. 30, No. 3, pp. 163-165.
[32] DU Jun, MA Yu-cai. Climatic Trend of Rainfall over Tibetan Plateau
from 1971 to 2000. Acta Geographica Sinica, 2004, vol. 59, No. 3, pp.
375-382.
[33] WU Shao-hong, YIN Yun-he, ZHENG Du, YANG Qin-ye. Climate
Changes in the Tibetan Plateau during the Last Three Decades. Acta
Geographica Sinica, 2005, vol. 60, No. 1, pp. 3-11.
[34] Chen Long-xun, Zhou Xiu-ji, Li Weiliang. Characteristics of the climate
change and its formation mechanism in China in last 80 years. Acta
Meteorologica Sinica, 2004, vol. 62, No. 5, pp. 634-646.
[35] Niu Tao, Chen Long-xun, Wang Wen. REOF analysis of climatic
characteristics of winter temperature and humidity on Xizang-Qinghai
Plateau. Journal of applied meteorological science, 2002, vol. 13, No.5,
pp. 560-570.
[36] ZHOU Zi-jiang , WANG Xi-wen, NIU Ruo-yun. Climate characteristics
of sandstorm in China in recent 47 years, Quarterly Journal of Applied
Meteorlolgy, 2002, vol. 13, No. 2, pp. 193-200.
[37] Jiang Ying, Luo Yong, Zhao Zong-ci. Projection of wind speed changes
in China in the 21st century by climate models. Chinese Journal of
Atmospheric Sciences, 2010, vol. 34, No. 2, pp. 323-336.
[38] Rayner D. Wind run changes: The dominant factor affecting pan
evaporation trends in Australia. Journal of Climate, 2007, vol. 20, No. 14,
pp. 3379-3394.
[39] Roderick M, Rotstayn L, Farquhar G, et al. On the attribution of changing
pan evaporation. Geophysical Research Letters, 2007, 34.L17403, doi:
10.1029/2007GL031166.
[40] MAO Fei, HOU Ying-yu, TANG Shi-hao,et al. Classification and
dynamic changes of grasslands in Northern Tibet based on recent 20 years
satellite data. Chinese Journal of Applied Ecology, 2007, vol. 18, No. 8,
pp. 1745-1750.
[1] Mo Hang-up, Zhang Bai-ping, Cheng Wei-ming, et al. Major environmental effects of the Tibetan plateau, Progress in Geography,
2004, vol. 23, No. 2, pp. 88-96.
[2] WANG Jing-sheng, ZHANG Xian-zhou, ZHAO Yu-ping, et al. Spatio-temporal pattern of climate changes in Northern Tibet-s Qiangtang
Plateau. Resources science, 2008, vol. 30, No. 12, pp. 1852-1859.
[3] WANG Nan, LI Dong-liang, ZHANG Jie. Research Advance of Surface
Temperature Change over Tibetan Plateau. Journal of Arid Meteorology,
2010, vol. 28, No. 3, pp. 265-269.
[4] Cramer W P,Leemans R. Assessing impacts of climate change vegetation
using climate classification system. In:Solomon A M, Shuart H H(eds.).
Vegetation Dynamics and Global Change, London: Chapman and Hall,
1993, pp. 190-217.
[5] ZHANG Yue-cong, ZHAO Zhi-qiang, LI Shuang-cheng. Indicating
variation of surface vegetation cover using SPOT NDVI in the northern
part of North China. Geographical Research,2008, vol. 27, No. 4, pp. 745-754.
[6] Pettorelli N, Vik J, Mysterud A, et al. Using the satellite derived NDVI to
assess ecological responses to environmental change. Trends in Ecology
& Evolution, 2005, vol. 20, No. 9, pp. 503-510.
[7] Ichii K, Kawabata A, Yamaguchi Y. Global correlation analysis for
NDVI and climatic variables and NDVI trends: 1982-1990 [J]. International Journal of Remote Sensing, 2002, vol. 23, No. 18, pp.
3873-3878.
[8] Piao S, Mohammat A, Fang J, et al. NDVI-based increase in growth of
temperate grasslands and its responses to climate changes in
China.Global Environmental Change,2006, vol. 16, No. 4, pp. 340-348.
[9] Ding M J, Zhang Y L, Liu L S, et al. The relationship between NDVI and
precipitation on the Tibetan Plateau. Journal of Geographical Sciences,
2007, vol. 17, No.3, pp. 259-268.
[10] Tucker C J, Pinzon J E, Brown M E, et al. An Extended AVHRR 8 km
NDVI data set compatible with MODIS and SPOT vegetation NDVI data.
Int. J. Remote Sensing, 2005, vol. 26, No. 20, pp. 4485-4498.
[11] LI Ben-gang, TAO Shu. Correlation between AVHRR NDVI and climate
factors. Acta Ecologica Sinica, 2000, vol. 20, No. 5, pp. 898~902.
[12] LI Xia, LI Xiao-bing, CHEN Yun-hao, et al. Temporal responses of
vegetation to climate variables in temperate steppe of northern China.
Journal of Plant Ecology, 2007, vol. 31, No. 6, pp. 1054-1062.
[13] Gao Z Q, Dennis O. The temporal and spatial relationship between NDVI
and climatological parameters in Colorado. Journal of Geographical
Sciences, 2001, vol. 11, No. 4, pp. 411-419.
[14] CHU Duo,DEJI Yang-zong,PUBU Ciren,et al. The response of typical
vegetation growth to climate conditions in North Tibetan Plateau. Journal
of applied meteorological science, 2007, vol. 18, No. 6, pp. 832-839.
[15] ZHAO Yu-ping, ZHANG Xian-zhou, WANG Jing-sheng, SHEN
Zhen-xi. Correlation Analysis between NDVI and Climatic Factors of
Grassland Ecosystems in the Northern Tibetan Plateau from 1982 to
2003. Resources Science, 2009, vol. 31, No. 11, pp. 1988-1998.
[16] DING Ming-jun, ZHANG Yi-li, LIU Lin-shan, WANG Zhao-feng,
YANG Xu-chao. Seasonal Time Lag Response of NDVI to Temperature
and Precipitation Change and Its Spatial Characteristics in Tibetan
Plateau, Progress in geography, 2010, vol. 29, No.4, pp. 507-512.
[17] MAO Fei, LU Zhi-guang, ZHANG Jia-hua, et al. Relations between
AVHRR NDVI and climate factors in Northern Tibet in recent 20 years.
Acta Ecolgica Sinica, 2007, vol. 27, No.8, pp. 3198-3205.
[18] Zheng Du. Study on natural geographical system of the Qinghai-Tibet
Plateau. Science in China (Series D), 1996, vol. 26, No. 4, pp. 336-341.
[19] LIA NG Si-hai, CHEN Jiang, JIN Xiao-mei, W AN Li, GONG Bin.
Regularity of Vegetation Coverage Changes in the Tibetan Plateau over
the Last 21 Years. Advance in earth science, 2007, vol. 22, No. 1, pp.
33-40.
[20] ZHANG Yi-li, LI Bing-yuan, ZHENG Du. A discussion on the boundary
and area of the Tibetan Plateau in China. Geographical Research, 2002,
vol. 21, No. 1, pp. 1-8.
[21] WEI F Y. Statistic diagnose and foreshadow technology in present
climate. Beijing: Meteorological Press, 1999, pp. 62-79.
[22] XU Z X,TAKEUCHI K,ISHIDAIRA H. Long—term trends of annual
temperature and precipitation time series in Japan. Journal of
Hydroscienee and Hydraulic Engineering, 2002, vol. 20, No. 2, pp. 11-26.
[23] ERCAN K,SERDAR K. Trend analysis of stream flow in Turkey. Journal
of Hydrology, 2004, vol. 289, pp. 128-144.
[24] JIANG Tong, SU Buda, WANG Yanjun, et al. Trends of Temperature,
Precipitation and Runoff in the Yangtze River Basin from 1961 to 2000.
Advances in Climate Change Research, 2005, vol.1, No. 2, pp. 65-68.
[25] Chen Yanli, Long Bu-ju, Pan Xue-biao, Mo Weihua. Grassland
Vegetation Change Based on MODIS NDVI Data and Climate
Information. Journal of Applied Meteorological Science, 2010, vol. 12,
No. 2, pp. 229-236.
[26] IPCC. Climate Change 2001: Impacts, adaptation, and vulnerability.
Summary for Policymakers. A Report of Working Group Ⅱ of the
Intergovernmental Panel on Climate Change. Geneva. Switzerland, 2001.
[27] IPCC. IPCC Fourth Assessment Report(AR4）,Cambridge: Cambridge
University Press, 2007.
[28] LIN Xue-chun, YU Shu-qiu, TANG Guo-li. Series of average air
temperature over China for the last 100-year period. Scientia
atmospherica sinica, 1995, vol. 19, No. 5, pp. 525-534.
[29] QIN Da-he. Colligate Report of Assessment in Environment Evolvement
of West at China. Beijing: Science Press, 2002, pp. 2-10.
[30] MA Xiao-bo, HU Ze-yong. Precipitation Variation Characteristics and
Abrupt Change over Qinhai-Xizang Plateau in Recent 40 Years. Journal
of Desert Research, 2005, vol. 25, No. 1, pp. 137-139.
[31] Yao Li, Wu Qing-mei. Climatic change of characteristics over
Qinghai-Xizang Plateau. Meteorological Science and Technology, 2002,
vol. 30, No. 3, pp. 163-165.
[32] DU Jun, MA Yu-cai. Climatic Trend of Rainfall over Tibetan Plateau
from 1971 to 2000. Acta Geographica Sinica, 2004, vol. 59, No. 3, pp.
375-382.
[33] WU Shao-hong, YIN Yun-he, ZHENG Du, YANG Qin-ye. Climate
Changes in the Tibetan Plateau during the Last Three Decades. Acta
Geographica Sinica, 2005, vol. 60, No. 1, pp. 3-11.
[34] Chen Long-xun, Zhou Xiu-ji, Li Weiliang. Characteristics of the climate
change and its formation mechanism in China in last 80 years. Acta
Meteorologica Sinica, 2004, vol. 62, No. 5, pp. 634-646.
[35] Niu Tao, Chen Long-xun, Wang Wen. REOF analysis of climatic
characteristics of winter temperature and humidity on Xizang-Qinghai
Plateau. Journal of applied meteorological science, 2002, vol. 13, No.5,
pp. 560-570.
[36] ZHOU Zi-jiang , WANG Xi-wen, NIU Ruo-yun. Climate characteristics
of sandstorm in China in recent 47 years, Quarterly Journal of Applied
Meteorlolgy, 2002, vol. 13, No. 2, pp. 193-200.
[37] Jiang Ying, Luo Yong, Zhao Zong-ci. Projection of wind speed changes
in China in the 21st century by climate models. Chinese Journal of
Atmospheric Sciences, 2010, vol. 34, No. 2, pp. 323-336.
[38] Rayner D. Wind run changes: The dominant factor affecting pan
evaporation trends in Australia. Journal of Climate, 2007, vol. 20, No. 14,
pp. 3379-3394.
[39] Roderick M, Rotstayn L, Farquhar G, et al. On the attribution of changing
pan evaporation. Geophysical Research Letters, 2007, 34.L17403, doi:
10.1029/2007GL031166.
[40] MAO Fei, HOU Ying-yu, TANG Shi-hao,et al. Classification and
dynamic changes of grasslands in Northern Tibet based on recent 20 years
satellite data. Chinese Journal of Applied Ecology, 2007, vol. 18, No. 8,
pp. 1745-1750.
@article{"International Journal of Earth, Energy and Environmental Sciences:50530", author = "Shen Weishou and Ji Di and Zhang Hui and Yan Shouguang and Li Haidong and Lin Naifeng", title = "The Response Relation between Climate Change and NDVI over the Qinghai-Tibet plateau", abstract = "Based on a long-term vegetation index dataset of NDVI and meteorological data from 68 meteorological stations in the Qinghai-Tibet plateau and their relations with major climate factors were analyzed. The results show the following: 1) The linear trends of temperature in the Qinghai-Tibet plateau indicate that the temperature in the plateau generally increased, but it rose faster in the last 20 years. 2) The most significant NDVI increase occurred in the eastern and southern plateau. However, the western and northern plateau demonstrate a decreasing trend. 3) There is a significant positive linear correlation between NDVI and temperature and a negative correlation between NDVI and mean wind speed. However, no significant statistical relationship was found between NDVI and relative humidity, precipitation or sunshine duration.4) The changes in NDVI for the plateau are driven by temperature-precipitation, but for the desert and forest areas, the relation changes to precipitation-temperature-wind velocity and wind velocity-temperature-precipitation.
", keywords = "Qinghai-Tibet plateau, NDVI, climate warming.", volume = "5", number = "11", pages = "649-7", }
