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Journal of Arid Land  2016, Vol. 8 Issue (2): 172-183    DOI: 10.1007/s40333-015-0060-x
Research Articles     
Oasis cold island effect and its influence on air temperature: a case study of Tarim Basin, Northwest China
HAO Xingming*, LI Weihong
State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China
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Abstract  Oasis effect can improve the regional climate and habitability of an arid region. In this study, we explored the cold island effects of oases distributed along the edge of Tarim Basin by analyzing the oasis cold island effect (OCIE) intensity, spatial-temporal variation of OCIE, factors influencing the OCIE and impacts of OCIE on air temperature using geographical statistics and GIS methods based on the MODIS land surface temperature, land use/cover change (LUCC) and observed air temperature data. Results showed that all the oases in the Tarim Basin exhibited cold island effects, with the OCIE intensity highest in summer (−9.08°C), followed by autumn (−4.24°C) and spring (−3.85°C). The total area of oasis cold island (OCI) and the comprehensive OCIE index showed the same seasonal change trend as the OCIE intensity. However, the changing trends in areas of OCI with strong, medium and weak OCIEs were inconsistent across different seasons. Farmland and water areas were found to be the key contributors that affected the OCIE, and the area and aggregation metrics of these two land use/cover types directly contributed to the OCIE. By contrast, natural vegetation, such as forest and grassland, almost had no contribution to the OCIE. Simulation of observed air temperature data showed that if farmland is replaced by forest or grassland in the oasis, the mean, maximum and minimum air temperatures will increase significantly. This heating effect will be higher in summer (reaching 1.14°C to 2.08°C) and lower in spring and autumn. Moreover, the heating effect of farmland being replaced by forest will be higher than that of farmland being replaced by grassland. These results can provide a basis for understanding the cold island effect of oases in arid regions.

Key wordsAstragalus caragana      Astragalus cyclophyllon      Astragalus podolobus      environmental factors      Maxent     
Received: 06 June 2015      Published: 01 April 2016
Fund:  

This work was funded by the National Natural Science Foundation of China (41571109).

Corresponding Authors:
Cite this article:

HAO Xingming, LI Weihong . Oasis cold island effect and its influence on air temperature: a case study of Tarim Basin, Northwest China. Journal of Arid Land, 2016, 8(2): 172-183.

URL:

http://jal.xjegi.com/10.1007/s40333-015-0060-x     OR     http://jal.xjegi.com/Y2016/V8/I2/172

Chen Y N, Chen Z S. 2013. Analysis of oasis evolution and suitable development scale for arid regions: a case study of the Tarim River Basin. Chinese Journal of Eco-Agriculture, 21(1): 134–140. (in Chinese)

Chu P C, Lu S H, Chen Y C. 2005. A numerical modeling study on desert oasis self-supporting mechanisms. Journal of Hydrology, 312(1–4): 256–276.

Fan Z L, Xia X C, Shen Y L, et al. 2002. Utilization of water resources, ecological balance and land desertification in the Tarim Basin, Xinjiang. Science in China Series D: Earth Sciences, 45(S1): 102–108.

Feng Q, Si J H, Zhang Y W, et al. 2006. Microclimatic characteristics of the Heihe oasis in the hyperarid zone of China. Journal of Geographical Sciences, 16(1): 34–44.

Han B, Lü S H, Ao Y H. 2010. Analysis on the interaction between turbulence and secondary circulation of the surface layer at Jinta Oasis in summer. Advances in Atmospheric Sciences, 27(3): 605–620.

Ji X B, Zhao W Z, Kang E S, et al. 2011. Carbon dioxide, water vapor, and heat fluxes over agricultural crop field in an arid oasis of Northwest China, as determined by eddy covariance. Environmental Earth Sciences, 64(3): 619–629.

Jiang L W, Tong Y F, Zhao Z J, et al. 2005. Water resources, land exploration and population dynamics in arid areas–the case of the Tarim River basin in Xinjiang of China. Population and Environment, 26(6): 471–503.

Li B F, Chen Y N, Shi X. 2012. Why does the temperature rise faster in the arid region of northwest China? Journal of Geophysical Research: Atmospheres (1984–2012), 117(D16): 16115, doi: 10.1029/2012JD017953.

Li W L, Lü S H, Fu S M, et al. 2011. Numerical simulation of fluxes generated by inhomogeneities of the underlying surface over the Jinta Oasis in Northwestern China. Advances in Atmospheric Sciences, 28(4): 887–906.

Liu B, Zhao W Z, Chang X X, et al. 2010. Water requirements and stability of oasis ecosystem in arid region, China. Environmental Earth Sciences, 59(6): 1235–1244.

Liu S H, Liu H P, Hu Y, et al. 2007. Numerical simulations of land surface physical processes and land-atmosphere interactions over oasis-desert/Gobi region. Science in China Series D: Earth Sciences, 50(2): 290–295.

Potchter O, Goldman D, Kadish D, et al. 2008. The oasis effect in an extremely hot and arid climate: the case of southern Israel. Journal of Arid Environments, 72(9): 1721–1733.

Qiu G Y, Li H Y, Zhang Q T, et al. 2013. Effects of evapotranspiration on mitigation of urban temperature by vegetation and urban agriculture. Journal of Integrative Agricluture, 12(8): 1307–1315.

Schwarz N, Lautenbach S, Seppelt R. 2011. Exploring indicators for quantifying surface urban heat islands of European cities with MODIS land surface temperatures. Remote Sensing of Environment, 115(12): 3175–3186.

Su C X, Hu Y Q. 1987. The structure of the oasis cold island in the planetary boundary layer. Acta Meteorologica Sinica, 45(3): 322–328. (in Chinese)

Taha H, Akbari H, Rosenfeld A. 1991. Heat island and oasis effects of vegetative canopies: micro-meteorological field-measurements. Theoretical and Applied Climatology, 44(2): 123–138.

Wan Z M, Li Z L. 1997. A physics-based algorithm for retrieving land-surface emissivity and temperature from EOS/MODIS data. IEEE Transactions on Geoscience and Remote Sensing, 35(4): 980–996.

Wen L J, Lü S H, Chen S Q, et al. 2005. Numerical simulation of cold island effect in Jinta Oasis summer. Plateau Meteorology, 24(6): 865–871. (in Chinese)

Yang F X, Mu G J, Yue J, et al. 2006. Formation causes and evolution of oases in arid areas. Arid Land Geography, 29(1): 70–75. (in Chinese)

Yang Y B, Su W Z, Jiang N. 2006. Time-space character analysis of urban heat island effect in Nanjing city using remote sensing. Remote Sensing Technology and Application, 21(6): 488–492. (in Chinese)

Zhang H, Wu J W, Zheng Q H, et al. 2003. A preliminary study of oasis evolution in the Tarim Basin, Xinjiang, China. Journal of Arid Environments, 55(3): 545–553.
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