Abstract
The observation data of ground stations is the main data source of this study. The data about the daily mean temperature, daily minimum temperature, daily precipitation, daily wind speed, and daily sunshine hours are from the meteorological observation database of National Meteorological Information Center in China Meteorological Administration (http://www.nmic.gov.cn/). The time span of meteorological data is mainly set from January 1, 1961 to December 31, 2008 in order to ensure the length of all data uniform and stable. It is necessary to select qualified observation data by the data quality control before analysis in order to ensure the accuracy of the results of the study. The quality control of meteorological observation data in this study is to examine the date of the daily mean temperature, daily minimum temperature, daily maximum temperature, and daily precipitation by using the international test method and software nonuniformity: RclimDex and RHtest, and to find out the station having data quality problems, then to delete them from the original data, finally, to select the qualified observation stations and to make a statistics and analysis on the basis of this data.
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References
Aguilar, E., et al. (2005). Changes in precipitation and temperature extremes in Central America and northern South America, 1961–2003. Journal Geophysical Research, 110(D23), 107.
Alexander, L. V., et al. (2006). Global observed changes in daily climate extremes of temperature and precipitation. Journal Geophysical Research, 111(D05), 109.
Dyurgerov, M. B. (2003). Mountain and subpolar glaciers show an increase in sensitivity to climate warming and intensification of the water cycle. Journal of Hydrology, 282, 164–176.
Easterling, D. R., & Peterson, T. C. (1995). A new method for detecting undocumented discontinuities in climatological time series. International Journal of Climatology, 15, 369–377.
Easterling, D. R., et al. (1997). Maximum and minimum temperature trends for the globe. Science, 277, 364–367.
Guo, Q. Y., et al. (2004). Studies on the variations of East-Asian summer monsoon during AD 1873–2000. Atmospheric Sciences, 28(2), 206–215. (in Chinese).
Heim, A. (1936). The glaciation and solifluction of MinyaGongkar. Geographical Journal, 87, 444–454.
Jones, P. D., et al. (2008). Urbanization effects in large-scale temperature records, with an emphasis on China. Journal Geophysical Research, 113, D16132.
Kistler, R., et al. (2001). The NCEP-NCAR 50-year reanalysis: monthly means CD-ROM and documentation. Bulletin of the American Meteorological society, 82, 247–267.
Kalnay, E., et al. (1996). The NCEP/NCAR 40-year reanalysis project. Bulletin of the American Meteorological society, 77, 437–471.
Li, J. J., & Su, Z. (1996). Glaciers in Hengduan Mountains. Beijing: Science Press. (in Chinese).
Li, Z. X., et al. (2010a). Changes of climate, glaciers and runoff in China’s monsoonal temperate glacier region during the last several decades. Quaternary International, 218(2010), 13–28.
Li, Z. X., et al. (2010b). Changes of the Hailuogou glacier, Mt. Gongga, China, against the background of climate change since the Holocene. Quaternary International, 2010(218), 166–175.
Li, Z. X., et al. (2008). Response of “glaciers-runoff” system in a typical temperate-glacier, Hailuogou glacier in Gongga Mountain of China to global change. Scientia Geographica Snica, 28(2), 229–234. (in Chinese).
Li, Z. X., et al. (2009a). Changes of some monsoonal temperate glaciersin Hengduan Mountains region during 1900–2007. Acta Geographica Sinica, 64(11), 1319–1330. (in Chinese).
Li, Z. X., et al. (2009b). Changes in Hailuogou during the recent 100 years under global warming. Journal Glaciology and Geocryology., 31(1), 75–81. (in Chinese).
Liu, B., et al. (2004). Taking China’s temperature: Daily range, warming trends, and regional variations, 1955–2000. Journal of Climate, 17, 4453–4462.
Li, Q. X., et al. (2004a). Urban heat island effect on annual mean temperature during the last 50 years in China. Theoretical and Applied Climatology, 79, 165–174.
Li, Q. X., et al. (2004b). Detecting and adjusting temporal inhomogeneity in Chinese mean surface air temperature data. Advances in Atmospheric Sciences, 21, 260–268.
Lund, R., & Reeves, J. (2002). Detection of undocumented change points: A revision of the two-phase regression model. Journal of Climate, 15, 2547–2554.
Liu, Q. (2005). Glacier variation and environmental evolution in Gongga Mountain. A master dissertation in Graduate University of Chinese Academy of Sciences. (in Chinese).
Ma, L. J., et al. (2008). Evaluation of ERA-40, NCEP-1, andNCEP-2 reanalysis air temperatures with ground-based measurements in China. Journal Geophysical Research, 113, D15115.
New, M., et al. (2006). Evidence of trends in daily climate extremes over southern and west Africa. Journal Geophysical Research, 111(D14), 102.
Pu, J. C. (1994). Glacier inventory of China VIII the Yangtze River system (pp. 117–129). Lanzhou: Gansu Culture Press. (in Chinese).
Ren, G., et al. (2008). Urbanization effects on observed surface air temperature trends in north China. Journal of Climate, 21, 1333–1348.
Shen, Y. P. (2000). The latest record of global glacier ablation under the material balance. Journal of Glaciology and Geocryology., 22(2), 105. (in Chinese).
Su, Z., et al. (2002). Quaternary glacial remains on the Gongga Mountain and the division of glacial period. Advance in Earth Sciences., 17(5), 639–647. (in Chinese).
Wu, Z. X. (2005). Analysis on observational data of meteorology in modern China. Meteorology, 31(1), 82–85. (in Chinese).
Wang, H. (2001). The weakening of the Asian monsoon circulation after the end of 1970’s. Advances in Atmospheric Sciences, 18, 376–386.
Wang, Y. Q., & Zhou, L. (2005). Observed trends in extreme precipitation events in China during 1961–2001 and the associated changes in large-scale circulation. Geophysical Research Letters, 32, L09707.
Wang, X. L. (2003). Comments on Detection of undocumented change points: A revision of the two-phase regression model. Journal of Climate, 16, 3383–3385.
Wang, S. W., et al. (1998). Construction of annual temperature series in China in recent hundred years. Journal of Applied Meteorological Science, 9(4), 392–401. (in Chinese).
Xu, M., et al. (2006). Steady decline of east Asian monsoon winds, 1969–2000: Evidence from direct ground measurements of wind speed. Journal Geophysical Research, 111, D24111.
Yang, Z. S., et al. (1994). The Application of Evaporation Ration (E/E_0) to the regionalization and classification of arid and humid climate of Yunnan Province. Journal of Yunnan University (Natural Sciences), 16(supplement), 91–98. (in Chinese).
Zhang, X. L., et al. (2004). Avoiding inhomogeneities in percentile-based indices of temperature extremes. Journal of Climate, 18, 1641–1651.
Zhang, W. J., et al. (2001). Response of Hailuogou present ice on climate change. The environment and ecosystem in the eastern edge of Qinghai-Xizang Plateau (pp. 111–118). Chengdu: Sichuan University Press. (in Chinese).
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Li, Z. (2015). Data and Methods. In: Study on Climate Change in Southwestern China. Springer Theses. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-44742-0_2
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DOI: https://doi.org/10.1007/978-3-662-44742-0_2
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