Abstract
Annually averaged daily maximum and minimum surface temperatures from southeastern China were evaluated for artificial discontinuities using three different tests for undocumented changepoints. Changepoints in the time series were identified by comparing each target series to a reference calculated from values observed at a number of nearby stations. Under the assumption that no trend was present in the sequence of target-reference temperature differences, a changepoint was assigned to the target series when at least two of the three tests rejected the null hypothesis of no changepoint at approximately the same position in the difference series. Each target series then was adjusted using a procedure that accounts for discontinuities in average temperature values from nearby stations that otherwise could bias estimates of the magnitude of the target series step change. A spatial comparison of linear temperature trends in the adjusted annual temperature series suggests that major relative discontinuities were removed in the homogenization process. A greater number of relative change points were detected in annual average minimum than in average maximum temperature series. Some evidence is presented which suggests that minimum surface temperature fields may be more sensitive to changes in measurement practice than maximum temperature fields. In addition, given previous evidence of urban heat island (i.e., local) trends in this region, the assumption of no slope in a target-reference difference series is likely to be violated more frequently in minimum than in maximum temperature series. Consequently, there may be greater potential to confound trend and step changes in minimum temperature series.
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References
Aguilar, E., I. Auer, M. Brunet, T. C. Peterson, and J. Wieringa, 2003: Guidance on metadata and homogeneity. WMO Publication TD No. 1186, World Meteorological Organization, Geneva. 50pp.
Akaike, H., 1974: A new look at the statistical identification model. IEEE Trans. Auto. Control, 19, 716–723.
Alexandersson, H., 1986: A homogeneity test applied to precipitation data. International Journal of Climatology, 6, 661–675.
Alexandersson, H., and A. Moberg, 1997: Homogenization of Swedish temperature data. Part I: Homogeneity test for linear trends. International Journal of Climatology, 17, 25–34.
Baker, D. G., 1975: Effect of observation time on mean temperature estimation. J. Appl. Meteor., 14, 471–476.
Caussinus, H., and O. Mestre, 2004: Detection and correction of artificial shifts in climate series. Journal Royal Statistical Societies Series C, 53(3), 405–425.
Chinese Meteorological Administration, 1979: The Rules of Surface Meteorological Observation. The Meteorological Press, Beijing, 186pp. (in Chinese)
Easterling, D. R., and T. C. Peterson, 1995: A new method for detecting and adjusting for undocumented discontinuities in climatological time series. International Journal of Climatology, 15, 369–377.
Easterling, D. R., and Coauthors, 1997: Maximum and minimum temperature trends for the globe. Science, 277, 364–367.
Gall, R., K. Young, R. Schotland, and J. Schmitz, 1992: The recent maximum temperature anomalies in Tucson: Are they real or an instrumental problem? J. Climate, 5, 657–665.
Guttman, N. B., and C. B. Baker, 1996: Exploratory analysis of the difference between temperature observations recorded by ASOS and conventional methods. Bull. Amer. Meteor. Soc., 77, 2865–2873.
Huang, J., X. Liu, and Q. Li, 2004: The study of relationship between heat island effect and population in cities over south of China. Journal of Tropical Meteorology, 20, 713–722. (in Chinese)
Hawkins, D. M., 1976: Point estimation of the parameters of a piecewise regression model. Appllied Statistics, 25, 51–57.
Hubbard, K. G., X. Lin, and E. A. Walter-Shea, 2001: The effectiveness of the ASOS, MMTS, Gill, and CRS air temperature radiation shields. J. Atmos. Oceanic Technol., 18, 851–864.
Jones, P. D., S. C. B. Raper, R. S. Bradley, H. F. Diaz, P. M. Kelly, and T. M. L. Wigley, 1986: Northern Hemisphere surface air temperature variations: 1851–84. J. Climate Appl. Meteor., 25, 161–179.
Jones, P. D., D. H. Lister, and Q. X. Li, 2008: Urbanization effects in large-scale temperature records, with an emphasis on China. J. Geophys. Res., 113, D16122: 1–12.
Karl, T. R., and C. N. Williams, 1987: An approach to adjusting climatological time series for discontinuous inhomogeneities. J. Climate Appl. Meteor., 26, 1744–1763.
Karl, T. R., G. Kukla, V. N. Razuvayev, M. J. Changery, R. G. Quayle, R. R. Heim, D. R. Easterliing, and C. B. Fu, 1991: Global warming: Evidence for asymmetric diurnal temperature change. Geophys. Res. Lett., 18, 2253–2256.
Li, Q., X. Liu, H. Zhang, T. C. Peterson, and D. R. Easterling, 2004a: Detecting and adjusting on temporal inhomogeneities in Chinese mean surface air temperature datasets. Adv. Atmos. Sci., 21, 260–268.
Li, Q., H. Zhang, X. Liu, and J. Huang, 2004b: UHI effect on annual mean temperature during recent 50 years in China. Theoritical and Appllied Climatology, 79, 165–174.
Liu, X., and Q. Li, 2003: Research on inhomogeneity tests of climate data series in China. Acta Meteorologica Sinica, 17, 492–502.
Lund, R., and J. Reeves, 2002: Detection of undocumented changepoints: A revision of the two-phase regression model. J. Climate, 15, 2547–2554.
Menne, M. J., and C. N. Williams, 2005: Detection of undocumented change points using multiple test statistics and composite reference series. J. Climate, 18, 4271–4286.
Oke, T. R., 1987: Boundary Layer Climates. 2nd ed., Routledge, London, 435pp.
Parker, D., 2004: Large-scale warming is not urban. Nature, 432, 290–290.
Peterson, T. C., and D. R. Easterling, 1994: Creation of homogeneous composite climatological reference series. International Journal of Climatology, 14, 671–680.
Peterson, T. C., Coauthors 1998: Homogeneity adjustments of in situ atmospheric climate data: A review. International Journal of Climatology, 18, 1493–1517.
Potter, K. W., 1981: Illustration of a new test for detecting a shift in mean in precipitation series. Monthly Weather Review, 109, 2040–2045.
Schwarz, G., 1978: Estimating the dimension of a model. Annals Statistics, 6, 461–464.
Skinner, W. R., and D. W. Gullett, 1993: Trends of daily maximum and minimum temperature in Canada during the past century. Climatology Bulletin, 27, 63–77.
Szentimrey, T., 1999: Multiple analyses of series for homogenization (MASH). Proc. Second Seminar for Homogenization of Surface Climatological Data, Budapest, Hungary WMO-TD No. 962, 27–46.
Solow, A. R., 1987: Testing for climate change: An application of the two-phase regression model. J. Climate Appl. Meteor., 26, 1401–1405.
Vincent, L., 1998: A technique for the identification of inhomogeneities in Canadian temperature series. J. Climate, 11, 1094–1104
Wang, X. L., 2003: Comments on “Detection of Undocumented Change points: A Revision of the Two-Phase Regression Model”. J. Climate, 16, 3383–3385.
Wang, X. L., 2008: Penalized maximal F-test for detecting undocumented mean-shift without trend-change. J. Atmos. Oceanic Technol., 19, 368–384
Wang, X. L., Q. H. Wen, and Y. Wu, 2007: Penalized maximal t-test for detecting undocumented mean change in climate data series. Journal of Applied Meteorological Climatology, 46, 916–931.
Yan, Z. W., C. Yang, and P. Jones, 2001: Influence of inhomogeneity on the estimation of mean and extreme temperature trends in Beijing and Shanghai. Adv. Atmos. Sci., 18, 309–321.
Zhai, P. M., and R. E. Eskridge, 1996: Analysis of inhomogeneities in radiosonde and humidity time series. International Journal of Climatology, 9, 884–894.
Zhou, L., R. E. Dickinson, Y. Tian, J. Fang, Q. Li, R.K. Kaufmann, C. J. Tucker, and R. B. Myneni, 2004: Evidence for a significant urbanization effect on climate in China. Proceedings of National Academy of Sciences of USA, 101, 9540–9544.
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Li, Q., Dong, W. Detection and adjustment of undocumented discontinuities in Chinese temperature series using a composite approach. Adv. Atmos. Sci. 26, 143–153 (2009). https://doi.org/10.1007/s00376-009-0143-8
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DOI: https://doi.org/10.1007/s00376-009-0143-8