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AGU: Geophysical Research Letters

 

Keywords

  • temperature layer
  • lapse rate
  • near surface

Index Terms

  • Global Change: Regional climate change
  • Global Change: Climate dynamics
  • Global Change: Climate variability
  • Global Change: Impacts of global change

Abstract

GEOPHYSICAL RESEARCH LETTERS, VOL. 34, L24705, 6 PP., 2007
doi:10.1029/2007GL031652

An examination of 1997–2007 surface layer temperature trends at two heights in Oklahoma

X. Lin

High Plains Regional Climate Center, University of Nebraska at Lincoln, Lincoln, Nebraska, USA

R. A. Pielke Sr.

Cooperative Institute for Research in Environmental Sciences and Department of Atmospheric and Oceanic Sciences, University of Colorado, Boulder, Colorado, USA

K. G. Hubbard

High Plains Regional Climate Center, University of Nebraska at Lincoln, Lincoln, Nebraska, USA

K. C. Crawford

Oklahoma Climatological Survey, University of Oklahoma, Norman, Oklahoma, USA

M. A. Shafer

Oklahoma Climatological Survey, University of Oklahoma, Norman, Oklahoma, USA

T. Matsui

Laboratory for Atmosphere NASA Goddard Space Flight Center, Greenbelt, Maryland, USA

Goddard Earth Science and Technology Center, University of Maryland Baltimore County, Baltimore, Maryland, USA

This study assesses near surface lapse rates and temperatures over the past decade at two heights from the Oklahoma Mesonet. A statistically significant change in lapse rate was detected of −0.21 ± 0.09°C (10 m)−1 per decade. The trend of nighttime lapse rate was about three times larger than the magnitude of trend of the daytime lapse rate. The lapse rate trends at the time of the daily maximum and minimum temperatures were larger during calm conditions. Significantly, changes of temperature trends at a single height were inconclusive when the data was not segmented by wind speed classes. For daily maximum and minimum station series at two heights, the temperature trends of these station series were the largest for daily minimum temperature at 1.5 m under calm conditions, and the second largest for daily minimum temperatures at 9.0 m under calm conditions. These observations document that monitoring long term near-surface daily minimum temperature trends at a single level on light wind nights will not produce the same trends as for long term temperature trends at other heights near the surface.

Received 10 August 2007; accepted 20 November 2007; published 22 December 2007.

Citation: Lin, X., R. A. Pielke Sr., K. G. Hubbard, K. C. Crawford, M. A. Shafer, and T. Matsui (2007), An examination of 1997–2007 surface layer temperature trends at two heights in Oklahoma, Geophys. Res. Lett., 34, L24705, doi:10.1029/2007GL031652.

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