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Journal of Arid Land  2015, Vol. 7 Issue (2): 251-263    DOI: 10.1007/s40333-014-0042-4
Research Articles     
Effects of climate change on phenology and primary productivity in the desert steppe of Inner Mongolia
Fang HAN1,2, Qing ZHANG1,3, Alexander BUYANTUEV4, JianMing NIU1,3, PengTao LIU1,2, XingHua LI2, Sarula KANG1, Jing ZHANG1,ChangMing CHANG1, YunPeng LI2
1 School of Life Sciences, Inner Mongolia University, Hohhot 010021, China;
2 Meteorological Bureau of Inner Mongolian, Hohhot 010051, China;
3 Sino-US Center for Conservation, Energy and Sustainability Science in Inner Mongolia (SUCCESS), Hohhot 010021, China;
4 Department of Geography and Planning, the State University of New York, NY 12222, USA
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Abstract  Variations in temperature and precipitation affect local ecosystems. Considerable spatial and temporal heterogeneity exists in arid ecosystems such as desert steppes. We analyzed the spatiotemporal dynamics of climate and vegetation phenology in the desert steppe of Inner Mongolia, China, using meteorological data from 11 stations (1961–2010) and phenology data from 6 ecological stations (2004–2012). We also estimated the gross primary production for the period of 1982–2009 and found that the annual mean temperature increased at a rate of 0.47ºC/decade during 1961–2010, with the last 10 years being consistently warmer than the 50-year mean. The most significant warming occurred in winters. Annual precipitation slightly decreased during the 50-year period, with summer precipitation experiencing the highest drop in the last 10 years, and spring precipitation, a rise. Spatially, annual precipitation increased significantly in the northeast and eastern central area of the region next to the typical steppe. From 2004 to 2012, vegetation green-up and senescence date advanced in the area, shortening the growing season. Consequently, the primary productivity of the desert steppe decreased along precipitation gradient from southeast to northwest. Temporally, productivity increased during the period of 1982–1999 and significantly decreased after 2000. Overall, the last decade witnessed the most dramatic climatic changes that were likely to negatively affect the desert steppe ecosystem. The decreased primary productivity, in particular, decreases ecosystem resilience and impairs the livelihood of local farmers and herdsmen.

Key wordssoil respiration      abiotic exchange      hypothetical system      incorporated model;missing carbon sink     
Received: 24 February 2014      Published: 10 April 2015
Fund:  

The study was supported by the State Key Basic Research Development Program of China (2012CB722201), the National Basic Research Program of China (31200414, 31060320 and 30970504), the National Basic Research Program of Inner Mongolia (2009ms0603) and the Earmarked Fund for Modern Agro-Industry Technology Research System.

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Cite this article:

Fang HAN, Qing ZHANG, Alexander BUYANTUEV, JianMing NIU, PengTao LIU, XingHua LI, Sarula KANG, Jing ZHANG,ChangMing CHANG, YunPeng LI. Effects of climate change on phenology and primary productivity in the desert steppe of Inner Mongolia. Journal of Arid Land, 2015, 7(2): 251-263.

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http://jal.xjegi.com/10.1007/s40333-014-0042-4     OR     http://jal.xjegi.com/Y2015/V7/I2/251

Almorox J, Hontoria C. 2004. Global solar radiation estimation using sunshine duration in Spain. Energy Conversion and Management, 45: 1529–1535.

Bachu S, Adams J. 2003. Sequestration of CO2 in geological media in response to climate change: capacity of deep saline aquifers to sequester CO2 in solution. Energy Conversion and Management, 44: 3151–3175.

Bai Y F, Han X G, Wu J G, et al. 2004. Ecosystem stability and compensatory effects in the Inner Mongolia grassland. Nature, 431: 181–184.

Bai Y F, Wu J G, Xing Q, et al. 2008. Primary production and rain use efficiency across a precipitation gradient on the Mongolia plateau. Ecology, 89: 2140–2153.

Chen X Q, Hu B, Yu R. 2005. Spatial and temporal variation of phenological growing season and climate change impacts in temperate eastern China. Global Change Biology, 11: 1118–1130.

Chen X Q, Li L. 2009. Relationship between phenology of L. chinensis grassland and meteorological factors. Acta Ecologica Sinica, 29: 5280–5290. (In Chinese)

Cleland E E, Chuine I, Menzel A, et al. 2007. Shifting plant phenology in response to global change. Trends in Ecology and Evolution, 22: 357–365.

Cornelissen J H, Van Bodegom P M, Aerts R, et al. 2007. Global negative vegetation feedback to climate warming responses of leaf litter decomposition rates in cold biomes. Ecology Letters, 10: 619–627.

Ding X H, Chen T Z. 2008. Climate change of Inner Mongolia during past 50 years. Meteorology Journal of Inner Mongolia, 3: 17–19. (In Chinese)

Edwards M, Richardson A J. 2004. Impact of climate change on marine pelagic phenology and trophic mismatch. Nature, 430: 881–884.

Fang J Y, Piao S L, Field C B, et al. 2003. Increasing net primary production in China from 1982 to 1999. Frontiers in Ecology and the Environment, 1: 293–297.

Fang J Y, Piao S L, Zhou L M, et al. 2005. Precipitation patterns alter growth of temperate vegetation. Geophysical Research Letters, 32: L21411.

Field C B, Behrenfeld M J, Randerson J T, et al. 1998. Primary production of the biosphere: integrating terrestrial and oceanic components. Science, 281: 237–240.

Gu R Y, Zhou W C, Bai M L, et al. 2012. Impacts of climate change on phenological phase of herb in the main grassland in Inner Mongolia. Acta Ecologica Sinica, 32: 767–776. (In Chinese)

Hicke J A, Asner G P, Randerson J T, et al. 2002. Satellite-derived increases in net primary productivity across North America, 1982–1998. Geophysical Research Letters, 29: 69-1–69-4.

Hou X Y, Han Y, Li Y H. 2012. The perception and adaptation of herdsmen to climate change and climate variability in the desert steppe region of northern China. Rangeland Journal, 34: 349–357.

Inner Mongolia-Ningxia Joint Inspection Group of Chinese Academy of Sciences. 1985. Vegetation of Inner Mongolia. Beijing: Science Publishing House. (In Chinese)

IPCC. 2007. Climate change 2007: the physical science basis. Agenda 6.

Li X L, Liang S L, Yu G R, et al. 2013. Estimation of gross primary production over the terrestrial ecosystems in China. Ecological Modelling, 261: 80–92.

Ma W H, He J S, Yang Y H, et al. 2010. Environmental factors covary with plant diversity–productivity relationships among Chinese grassland sites. Global Ecology and Biogeography, 19: 233–243.

Menzel A. 2000. Trends in phenological phases in Europe between 1951 and 1996. International Journal of Biometeorology, 44: 76–81.

Menzel A, Sparks T H, Estrella N, et al. 2006. European phenological response to climate change matches the warming pattern. Global Change Biology, 12: 1969–1976.

Myneni R B, Keeling C, Tucker C, et al. 1997. Increased plant growth in the northern high latitudes from 1981 to 1991. Nature, 386: 698–702.

Nemani R R, Keeling C D, Hashimoto H, et al. 2003. Climate-driven increases in global terrestrial net primary production from 1982 to 1999. Science, 300: 1560–1563.

Piao S L, Fang J Y, Zhou L M, et al. 2005. Changes in vegetation net primary productivity from 1982 to 1999 in China. Global Biog¬eochemical Cycles, 19.

Piao S L, Mohammat A, Fang J Y, et al. 2006. NDVI-based increase in growth of temperate grasslands and its responses to climate changes in China. Global Environmental Change, 16: 340–348.

Piao S L, Fang J Y, Ciais P, et al. 2009. The carbon balance of terrestrial ecosystems in China. Nature, 458: 1009–1013.

Ren G Y, Guo J, Xu M Z, et al. 2005. Characteristics of terrestrial climate change in China during past 50 years. Meteorological Bulletin, 942–956. (In Chinese)

Ruimy A, Saugier B, Dedieu G. 1994. Methodology for the estimation of terrestrial net primary production from remotely sensed data. Journal of Geophysical Research: Atmospheres, 99: 5263– 5283.

Shi Y F, Shen Y P, Li D L, et al. 2003. Discussion on the present climate change from warm-dry to warm-wet in northwest China. Quaternary Sciences, 23: 152–164. (In Chinese)

Solomon S. 2007. Climate Change 2007: Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge: Cambridge University Press.

Sparks T, Carey P. 1995. The responses of species to climate over two centuries: an analysis of the Marsham phenological record, 1736–1947. Journal of Ecology, 83: 321–329.

Stenseth N C, Mysterud A, Ottersen G, et al. 2002. Ecological effects of climate fluctuations. Science, 297: 1292–1296.

The National Climate Change Assessment Report Writing Committee. 2007. The National Climate Change Assessment Report. Beijing: Science Press. (In Chinese)

Walther G R, Post E, Convey P, et al. 2002. Ecological responses to recent climate change. Nature, 416: 389–395.

Yuan W P, Liu S G, Zhou G S, et al. 2007. Deriving a light use efficiency model from eddy covariance flux data for predicting daily grossprimary production across biomes. Agricultural and Forest Meteorology, 143: 189–207.

Yuan W P, Liu S G, Yu G R, et al. 2010. Global estimates of evapo-transpiration and gross primary production based on MODIS and global meteorology data. Remote Sensing of Environment, 114: 1416–1431.

Yuan W P, Liu D, Dong W J, et al. 2013. Multiyear precipitation reduction strongly decrease carbon uptake over North China. Biogeosciences Discussions, 10: 1605–1634.

Yun W L, Hou Q, Wulanbateer. 2008. Impacts of climate change over last 50 years on net primary productivity in typical steppe of Inner Mongolia. Chinese Journal of Agrometeorology, 29: 294–297. (In Chinese)

Zhang C H, Wang M J, Zhang L, et al. 2013. Responses of aboveground net primary productivity to climate change in Hulunbel meadow grassland. Acta Prataculturae Sinica, 41–50. (In Chinese)

Zhang F, Zhou G S, Wang Y, et al. 2012. Evapotranspiration and crop coefficient for a temperate desert steppe ecosystem using eddy covariance in Inner Mongolia, China. Hydrological Processes, 26: 379–386.
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