Zobrazeno 1 - 10
of 135
pro vyhledávání: '"Henry Stommel"'
Autor:
Henry Stommel, Harlow G. Farmer
Publikováno v:
Journal of Marine Research. 79:91-98
A theoretical reason is developed to explain why the mouth of a vertically stratified estuary should act as a constraint on the amount of salt water available for mixing in the estuary. Flume experiments designed to test this idea are described. The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::38c103f859179b2050ced86c8a66ea1d
https://doi.org/10.1357/002224021834614380
https://doi.org/10.1357/002224021834614380
Autor:
Henry Stommel
This title is part of UC Press's Voices Revived program, which commemorates University of California Press's mission to seek out and cultivate the brightest minds and give them voice, reach, and impact. Drawing on a backlist dating to 1893, Voices Re
Autor:
Henry Stommel
Hundreds of islands that once appeared on nautical charts and general atlases are now known to have vanished — or never even existed. How were they detected in the first place? Henry Stommel, an oceanographer and senior scientist at Massachusetts'W
Publikováno v:
Tellus A; Vol 12, No 2 (1960)
Laboratory experiments which supplement those presented by Stommel, Arons and Faller (1958) are described. Extension of the analysis to include the effects of bottom friction shows that the characteristic spreading of zonal currents, apparent in the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f18e1d958c1d15e9d20ada3dc586bd53
http://www.tellusa.net/index.php/tellusa/article/view/9380
http://www.tellusa.net/index.php/tellusa/article/view/9380
Publikováno v:
Tellus A; Vol 10, No 2 (1958)
A simple regime of fluid flow is defined. This regime can occur in a homogeneous layer of fluid (i) of uniform depth on a rotating sphere and bounded by meridional barriers (ii) of uniform depth on a betaplane and bounded by barriers running north-so
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2ece7d0c27d6d59b1e979a835029faa4
http://www.tellusa.net/index.php/tellusa/article/view/9238
http://www.tellusa.net/index.php/tellusa/article/view/9238
Autor:
Henry Stommel
Publikováno v:
Tellus A; Vol 13, No 2 (1961)
Free convection between two interconnected reservoirs, due to density differences maintained by heat and salt transfer to the reservoirs, is shown to occur sometimes in two different stable regimes, and may possibly be analogous to certain features o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::621ff0a765e0b268388f641c79fb5d11
http://www.tellusa.net/index.php/tellusa/article/view/9491
http://www.tellusa.net/index.php/tellusa/article/view/9491
Publikováno v:
Journal of Physical Oceanography. 23:1885-1892
Because the volumetric census of deep and bottom water in the North Atlantic Ocean consists of three isolated linear ridges along which heat and salt flow through the main volumetric mode (and point of intersection), it is possible to deduce the expe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6a36cbd92f546c4ec43adc57413590e3
https://doi.org/10.1175/1520-0485(1993)023<1885:otsona>2.0.co
https://doi.org/10.1175/1520-0485(1993)023<1885:otsona>2.0.co
Autor:
Joseph Pedlosky, Henry Stommel
Publikováno v:
Journal of Physical Oceanography. 23:1800-1808
The authors describe a self-sustaining baroclinic inertial oscillation whose energy source rests in a uniform horizontal temperature gradient. This energy is released through the agency of a stratification-dependent mixing law that is meant to crudel
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::94cee168dac259fc63429fc0cf875218
https://doi.org/10.1175/1520-0485(1993)023<1800:ssio>2.0.co
https://doi.org/10.1175/1520-0485(1993)023<1800:ssio>2.0.co
Autor:
Henry Stommel
Publikováno v:
Journal of Physical Oceanography. 23:142-148
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6e2f65562d69fec6315f3b66f23b584c
https://doi.org/10.1175/1520-0485(1993)023<0142:acrmfd>2.0.co
https://doi.org/10.1175/1520-0485(1993)023<0142:acrmfd>2.0.co