Zobrazeno 1 - 10 of 31 pro vyhledávání: '"E. B. Kraus"'
1
Subtropical Droughts and Cross-Equatorial Energy Transports
Autor: E. B. Kraus
Publikováno v: Monthly Weather Review. 105:1009-1018
The spatial coherence of subtropical rainfall anomalies is documented by variance analysis. Major droughts repeatedly were felt at the same time around the globe along the arid margins of the tropical rainfall belt. The persistence of anomalies becom
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::c5b558acf787d42fd4ec837e2fa71c63
https://doi.org/10.1175/1520-0493(1977)105<1009:sdacee>2.0.co
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2
The Seasonal Excursion of the Intertropical Convergence Zone
Autor: E. B. Kraus
Publikováno v: Monthly Weather Review. 105:1052-1055
A simple analytical model relates the seasonal excursion of the Intertropical Convergence Zone to seasonal changes in hemispheric forcing. The maximum value of the excursion increases with the seasonal heating change; it decreases with the equator-po
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::aa9f5d0b7aba4c853b4f1be9045ee48b
https://doi.org/10.1175/1520-0493(1977)105<1052:tseoti>2.0.co
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3
Climatological aspects of the tropical convective boundary layer
Autor: E. B. Kraus, Howard P. Hanson
Publikováno v: Boundary-Layer Meteorology. 6:219-233
The characteristics of a boundary layer depend both on conditions at the surface and in the interior of the medium. In the undisturbed tropics, the latter are largely determined by subsidence and by infrared radiational cooling. One-dimensional model
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::51d77c910751aa22a7a42b91ac67837d
https://doi.org/10.1007/bf00232486
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4
Ocean Surface Drift Velocities
Autor: E. B. Kraus
Publikováno v: Journal of Physical Oceanography. 7:606-609
Symmetry considerations indicate that in steady-state conditions, and in the absence of a sea current, a horizontal interface must move in the direction of the surface geostrophic wind. With currents present, the interface velocity is the vector mean
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::7b4030b08732247304bb41ea84242394
https://doi.org/10.1175/1520-0485(1977)007<0606:osdv>2.0.co
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6
what do we not know about the sea-surface wind stress1
Autor: E. B. Kraus
Publikováno v: Bulletin of the American Meteorological Society. 49:247-253
A simple sampling experiment gives a several octave range of values for the zonal surface stress obtainable from synoptic maps over the North Atlantic. Uncertainty about the value of the drag coefficient account for about half the variance. The diffe
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::5205aa689ef9b1d5532153669b3f956e
https://doi.org/10.1175/1520-0477-49.3.247
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10
A discussion of the cell and parcel formulations of the convection problem
Autor: C. H. B. Priestley, E. B. Kraus
Publikováno v: Geofisica Pura e Applicata. 51:199-204
It is shown that there is a close mathematical similarity between the cell and parcel formulations of the convection problem, and analogies are drawn between some of the more significant properties of the solutions in the two cases.
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::b4eda51f6f60144bd93ceb3be6edf544
https://doi.org/10.1007/bf01992661
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