Zobrazeno 1 - 10
of 27
pro vyhledávání: '"G. E. Birchfield"'
Autor:
G. E. Birchfield, Huaxiao Wang
Publikováno v:
Climate Dynamics. 8:49-53
Latitudinal heat transport in the ocean and atmosphere represents a fundamental process of the Earth's climate system. The ocean component of heat transport is effected by the thermohaline circulation. Changes in this circulation, and hence latitudin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fcba53ae294085b5cc25874ce6eae73e
https://doi.org/10.1007/bf00209343
https://doi.org/10.1007/bf00209343
Publikováno v:
SEPM Journal of Sedimentary Research. 67
The limestone/marlstone bedding couplets of the Bridge Creek Limestone Member, Cenomanian-Turonian Greenhorn Formation, were analyzed by applying spectral techniques to high-resolution lithologic and geochemical data from a core. The results suggest
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bc2599b0cba9bcd2edb39b261358c2c9
https://doi.org/10.1306/d4268554-2b26-11d7-8648000102c1865d
https://doi.org/10.1306/d4268554-2b26-11d7-8648000102c1865d
Autor:
G. E. Birchfield, Johannes Weertman
Publikováno v:
Icarus. 50:462-472
Using the atmosphere-hydrosphere component of a paleoclimate model, the model sensitivity on a short time scale to changes in the parameterization of the surface albedo is examined in the context of response to orbitally produced insolation anomalies
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c6eba994a707a0cba032d3f2575049fe
https://doi.org/10.1016/0019-1035(82)90136-1
https://doi.org/10.1016/0019-1035(82)90136-1
Autor:
G. E. Birchfield, J. Weertman
Publikováno v:
Journal of Glaciology. 29:20-27
The theory of Nye and of Weertman of traveling waves on glaciers is extended to cover the situation where the presence of abundant basal water or increased basal water pressure produces increased sliding of a glacier over its bed. It is found that th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::af29a4c9874f3d1811ecb92be3a41a48
https://doi.org/10.1017/s0022143000005116
https://doi.org/10.1017/s0022143000005116
Autor:
J. Weertman, G. E. Birchfield
Publikováno v:
Journal of Glaciology. 29:374-382
Walder recently analyzed the initial instability of water flow in a sheet under a glacier that is produced by greater heat production in the flowing water and thus the larger rate of ice melting where a perturbation has increased the water sheet thic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7c11022f1592b12b08016f09ebc15073
https://doi.org/10.3189/s002214300003029x
https://doi.org/10.3189/s002214300003029x
Autor:
G. E. Birchfield, Isabelle Muszynski
Publikováno v:
Journal of Glaciology. 33:3-15
Evidence as to the potential roles of marine ice flows in the dramatic climatological changes which have occurred from the late Pleistocene to the present is reviewed, indicating the need for careful modeling studies to evaluate several crucial hypot
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1981627124e46e8a924fb9b54abacd7b
https://doi.org/10.3189/s0022143000005281
https://doi.org/10.3189/s0022143000005281
Publikováno v:
Quaternary Research. 15:126-142
A model for predicting the growth and decay of ice sheets based on the astronomical theory of climate change is presented. The purpose of the study in part is to isolate the role of the ice-sheet physics and earth response under varying ice load by s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e239cb56c9aff3638a01bde2bee69dba
https://doi.org/10.1016/0033-5894(81)90100-9
https://doi.org/10.1016/0033-5894(81)90100-9
Autor:
Isabelle Muszynski, G. E. Birchfield
Publikováno v:
Tellus A; Vol 37, No 2 (1985)
A study of antarctic accumulaton, surface temperature and elevation data reveals a strong correlation between the accumulation rate and the surface temperature which, in turn, is almost uniquely determined by the elevation of the ice sheet surface. T
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bbff2b5c28088e9068f11147051a26a7
https://doi.org/10.1111/j.1600-0870.1985.tb00282.x
https://doi.org/10.1111/j.1600-0870.1985.tb00282.x
Autor:
Brian P. Hickie, G. E. Birchfield
Publikováno v:
Journal of Physical Oceanography. 7:691-701
By solving an initial value problem, the time-dependent response of a large circular model lake to a steady wind stress has been investigated. Bottom stress has been neglected. The forced response has been divided naturally into a “seiche” respon
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cb4f7856e63e9e9437b2e613735275aa
https://doi.org/10.1175/1520-0485(1977)007<0691:ttdroa>2.0.co
https://doi.org/10.1175/1520-0485(1977)007<0691:ttdroa>2.0.co
Publikováno v:
Journal of the Atmospheric Sciences. 39:71-87
The response of a combined global zonal-averaged energy balance model and a continental ice-sheet model to insulation anomalies produced by orbital perturbations is examined. Although the role of ice sheet dynamics is included in the model, this pape
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::33c968ca9cf400fe44f6ca3db2f06cbc
https://doi.org/10.1175/1520-0469(1982)039<0071:amsotr>2.0.co
https://doi.org/10.1175/1520-0469(1982)039<0071:amsotr>2.0.co