Summary
Climate parameters are usually collected on some grid or pattern that is supposed to represent the unobserved neighborhood. Spatial dependence is a measure of the extent to which observed data represent the unobserved neighborhood. Geostatistical analyses provide procedures for measuring spatial dependence. In this study, semivariograms were estimated from hourly observations of screen-height air temperature obtained from a dense meteorological observation network. The range and spatial component normalized by the sill were estimated from the semivariogram in order to obtain information on the spatial structure of the air temperature. Zones of spatial correlation were delineated, using the range of the semivariogram. Scales of spatial correlation depended on the regional mean air temperature and regional wetness at the ground. The range or spatial scale for data collected in winter was larger than those in summer. The range under wet conditions was larger than under dry conditions. Effects of regional wind speed on range were different, depending on the regional mean air temperature. The normalized spatial component was used as an index for measuring continuities on the interpolation surface. The normalized spatial component generally increased as the range increased.
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References
Bergman, K. H., 1979: Multivariate analysis of temperatures and winds using optimum interpolation.Mon. Wea. Rev. 107, 1423–1444.
Blanchard, B. J., McFarland, M. J., Schmugge, T. J., Rhodes, E., 1981: Estimation of soil moisture with API algorithm and microwave emission.Water Resour. Bull. 17, 767–774.
Carlson, T. N., 1986: Regional-scale estimates of surface moisture availability in thermal inertia using remote thermal measurements.Remote Sens. Rev. 1, 197–247.
Choudhury, B., Blanchard, B., 1983: Simulating soil water recession coefficients for agricultural watersheds.Water Resour. Bull. 19, 241–247.
Delhomme, J. P., 1978: Kriging in the hydrosciences.Adv. Water Resour. 1, 251–266.
Hoel, P. G., 1976:Elementary Statistics 4th ed. New York: Wiley, 361 pp.
Journel, A. G., Huijbregts, Ch. J., 1978:Mining Geostatics. New York: Academic Press, 600 pp.
Julian, P. R., Thiebaux, H. J., 1975: On some properties of correlation functions used in optimum interpolation scheme.Mon. Wea. Rev. 103, 605–613.
Krige, D. E., 1966: Two-dimensional weighted moving average trend surfaces for ore-evaluation.J. South Africa Institution of Mining and Metallurgy 66, 13–38.
Linsley, R. K. Jr., Kohler, M. A., Paulhus, J. L. H., 1982:Hydrology for Engineers, 3rd ed. Tokyo: McGraw-Hill, 508 pp.
Lorenc, A., 1981: A global three-dimensional multivariate statistical interpolation scheme.Mon. Wea. Rev. 109, 701–721.
Mahrt, L., Gamage, N., 1987: Observations of turbulence in stratified flow.J. Atmos. Sci. 44, 1106–1121.
Matheron, G., 1963: Principles of geostatistics.Econ. Geol. 58, 1246–1266.
Mulla, D. J., 1988: Estimating spatial patterns in water content, matric suction, and hydraulic conductivity.Soil Sci. Soc. Am. J. 52, 1547–1553.
Orlanski, J., 1975: A rational subdivision of scales for atmospheric process.Bull. Amer. Meteor. Soc. 56, 527–530.
Powell, M. J. D., 1964: An efficient method for finding the minimum of a function of several variables without calculating derivatives.Computer J. 7, 155–162.
Price, J. C., 1985: On the analysis of thermal infra-red imagery: The limited utility of apparent thermal inertia.Remote Sensing Environ. 18, 59–73.
Sivakumar, M. V. K., Hartifield, J. L., 1990: Spatial variability of rainfall at an experimental station in Niger, West Africa.Theor. Appl. Climatol. 42, 33–39.
Smith, R. C. G., Prathapar, S. A., Barrs, H. D., 1989: Use of a thermal scanner image of a water stressed crop to study soil spatial variability.Remote Sensing Environ. 29, 111–120.
Tarpley, J. D., 1988: Some climatological aspects of satellite observed surface heating in Kansas.J. Appl. Meteor. 27, 20–29.
Tronci, N., Molteni, F., Bozzini, M., 1986: A comparison of local approximation methods for the analysis of meteorological data.Arch. Met. Geoph. Biocl., Ser. B 36, 189–211.
Vauclin, M., Vieira, S. R., Berbard, R., Hatfield, J. L., 1982: Spatial variability of surface temperature along two transects of a bare soil.Water Resour. Res. 18, 1677–1686.
Webster, R., Oliver, M. A., 1990:Statistical Methods in Soil and Land Resource Survey. New York: Oxford Univ. Press, 316 pp.
Wetzel, P. J., Atlas, D., Woodward, R. H., 1984: Determining soil moisture from geosynchronous satellite infrared data: A feasibility study.J. Appl. Meteor. 23, 375–390.
Willmott, C. J., 1987: Models, Climatic. In: Oliver, J. E., Fairbridge, R. W. (eds)Encyclopedia of Climatology. New York: Van Nostrand Reinhold, 584–590.
Yost, R. S., Uehara, G., Fox, R. L., 1982: Geostatistical analysis of soil chemical properties of large land areas. I, Semi-variograms.Soil Sci. Soc. Am. J. 46, 1028–1037.
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Kawashima, S., Ishida, T. Effects of regional temperature, wind speed and soil wetness on spatial structure of surface air temperature. Theor Appl Climatol 46, 153–161 (1992). https://doi.org/10.1007/BF00866095
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DOI: https://doi.org/10.1007/BF00866095