Nonstandard thermometer exposures at U.S. cooperative weather stations during the late nineteenth century
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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).”
From The Global Historical Climatology Network Monthly Temperature Dataset, Version 4 (2018) · cites this paper as Chenoweth 1993
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
Our analysis of the coupled feedbacks is entirely consistent with ICM (Zebiak 1993) and HCM studies (Latif and Barnett 1995; Nobre et al. 2003), which indicate that a damped coupled mode exists in the equatorial Atlantic.
“Our analysis of the coupled feedbacks is entirely consistent with ICM (Zebiak 1993) and HCM studies (Latif and Barnett 1995;Nobre et al. 2003), which indicate that a damped coupled mode exists in the equatorial Atlantic.”
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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