Cited by 90

Nonstandard thermometer exposures at U.S. cooperative weather stations during the late nineteenth century

Chenoweth, Michael·1993·Journal of Climate

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Crossref · 10.1175/1520-0442(1993)006<1787:nteauc>2.0.co;2

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  • The exposure characteristics of nineteenth century pre-Stevenson screen installations had a positive bias relative to instruments installed in Stevenson screens.

    “The exposure characteristics of the nineteenth century pre-Stevenson screen installations have been shown to have had a positive bias relative to instruments installed in the Stevenson screens, which provide more consistent protection from direct solar radiation (Chenoweth 1993; Parker 1994).”
  • In the Atlantic, eastern Atlantic SSTA and western Atlantic winds are related.

    “In the Atlantic it has been also long recognized that eastern Atlantic SSTA and western Atlantic winds are related (Servain et al. 1982;Hirst and Hastenrath 1983;Zebiak 1993).”

    From Understanding equatorial atlantic interannual variability (2007) · cites this paper as Zebiak 1993

  • Analysis of observations in the Atlantic indicates a link between SST and surface winds to the west, and the structure of the wind response is similar to that in the Pacific.

    “Analysis of observations in the Atlantic indicates that there is a link between SST and surface winds to the west (Servain et al. 1982;Hirst and Hastenrath 1983), and that the structure of the response in the wind field is similar to that in the Pacific (Zebiak 1993).”

    From Understanding equatorial atlantic interannual variability (2007) · cites this paper as Zebiak 1993

  • The Zebiak (1993) intermediate complexity model of the Atlantic simulates a coupled mode with a period of 4 yr, with similar physics to ENSO but strongly damped and only sustained by external forcing.

    “The Zebiak (1993) intermediate complexity model (ICM) of the Atlantic simulates a coupled mode with a period of 4 yr.”

    From Understanding equatorial atlantic interannual variability (2007) · cites this paper as Zebiak 1993

  • The equatorial Atlantic mode differs from ENSO in having significantly weaker variability, a much shorter duration (3 months) of extreme warm/cold events, and spectral characteristics hardly discernible from red noise.

    “The main differences to ENSO are the significantly weaker variability, the much shorter duration (3 months) of extreme warm/cold events, and spectral characteristics hardly discernable from red noise (Zebiak 1993;Carton and Huang 1994;Latif and Grötzner 2000).”

    From Understanding equatorial atlantic interannual variability (2007) · cites this paper as Zebiak 1993

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Authors
Chenoweth, M.
Venue
Journal of Climate
Published
1993
References
1

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