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R J Harding

Biographic Data

ID4342113
NAMER J Harding
GIVEN NAMESR J
FAMILY NAMEHarding
SIGNATUREHARDING R J
AFFILIATIONSUK Centre for Ecology & Hydrology
VERIFIEDNo
TOTAL WORKS2
TOTAL CITATIONS2
AUTHOR COUNT2
EDITOR COUNT0
FIRST PUBLICATION YEAR1980
LATEST PUBLICATION YEAR2012
H-INDEX1
  • Obstacles to data access for research related to climate and water

    Open Access•M Beniston, Markus Stoffel et al.•ARTICLE•Environmental Science & Policy•2012•Cited by: 1•References: 2

  • Altitudinal Gradients of Soil Temperatures in Europe

    F H W Green, R J Harding•ARTICLE•Transactions of the Institute of…•1980•Cited by: 1•References: 1

    The altitudinal gradient of soil temperature is examined with the aid of observations from ten countries in Europe. It is shown that this altitudinal gradient is always greatest in summer and least in winter, and that only the amplitude of the seasonal variation differs from one region to another. The altitudinal gradient of air temperature does not show the same degree of consistency, but in all cases it is in summer less than that of the soil. …

  • Obstacles to data access for research related to climate and water

    Open Access•M Beniston, Markus Stoffel et al.•ARTICLE•Environmental Science & Policy•2012•Cited by: 1•References: 2

  • Altitudinal Gradients of Soil Temperatures in Europe

    F H W Green, R J Harding•ARTICLE•Transactions of the Institute of…•1980•Cited by: 1•References: 1

    The altitudinal gradient of soil temperature is examined with the aid of observations from ten countries in Europe. It is shown that this altitudinal gradient is always greatest in summer and least in winter, and that only the amplitude of the seasonal variation differs from one region to another. The altitudinal gradient of air temperature does not show the same degree of consistency, but in all cases it is in summer less than that of the soil. …

  • Altitudinal Gradients of Soil Temperatures in Europe

    F H W Green, R J Harding•ARTICLE•Transactions of the Institute of…•1980•Cited by: 1•References: 1

    The altitudinal gradient of soil temperature is examined with the aid of observations from ten countries in Europe. It is shown that this altitudinal gradient is always greatest in summer and least in winter, and that only the amplitude of the seasonal variation differs from one region to another. The altitudinal gradient of air temperature does not show the same degree of consistency, but in all cases it is in summer less than that of the soil. …

  • Obstacles to data access for research related to climate and water

    Open Access•M Beniston, Markus Stoffel et al.•ARTICLE•Environmental Science & Policy•2012•Cited by: 1•References: 2

Botany and Plant Ecology Studies (1 works) · Business (1 works) · Computer Science (1 works) · Data access (1 works) · Data management (1 works) · Database (1 works) · demographic modeling and climate adaptation (1 works) · Economics (1 works) · Environmental economics (1 works) · Environmental resource management (1 works)

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