Zobrazeno 1 - 10
of 59
pro vyhledávání: '"R J Graham"'
Autor:
R. J. Graham, R. T. Pierrehumbert
Publikováno v:
The Astrophysical Journal, Vol 970, Iss 1, p 32 (2024)
Implicit in the definition of the classical circumstellar habitable zone (HZ) is the hypothesis that the carbonate-silicate cycle can maintain clement climates on exoplanets with land and surface water across a range of instellations by adjusting atm
Externí odkaz:
https://doaj.org/article/db148f3934994748b8ee7ba041a655ff
Autor:
N. P. Pinto, A. B. Maddux, L. A. Dervan, A. G. Woodruff, J. M. Jarvis, S. Nett, E. Y. Killien, R. J. Graham, K. Choong, P. M. Luckett, J. A. Heneghan, K. Biagas, E. F. Carlton, M. E. Hartman, L. Yagiela, K. N. Michelson, J. C. Manning, D. A. Long, J. Lee, B. S. Slomine, S. R. Beers, T. Hall, B. M. Morrow, K. Meert
Publikováno v:
Pediatric Critical Care Medicine. 23
Publikováno v:
Planetary Science Journal, 2(5):207
The Planetary Science Journal
The Planetary Science Journal
Central stages in the evolution of rocky, potentially habitable planets may play out under atmospheric conditions with a large inventory of non-dilute condensable components. Variations in condensate retention and accompanying changes in local lapse
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c8c0ab9d2cb33f13f1936f3dd9a92395
https://research.rug.nl/en/publications/e1dc063b-624b-4b08-9484-ea30c7cc1e50
https://research.rug.nl/en/publications/e1dc063b-624b-4b08-9484-ea30c7cc1e50
Autor:
R. J. Graham
The nearly logarithmic radiative impact of CO$_2$ means that planets near the outer edge of the liquid water habitable zone (HZ) require $\sim$10$^6$x more CO$_2$ to maintain temperatures conducive to standing liquid water on the planetary surface th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a65a540b76f69804d700119ce310718c
http://arxiv.org/abs/2104.01224
http://arxiv.org/abs/2104.01224
Autor:
Tiffany A. Shaw, R. J. Graham
Simulations show that storm tracks were weaker during past cold, icy climates relative to the modern climate despite increased surface baroclinicity. Previous work explained the weak North Atlantic storm track during the Last Glacial Maximum using dr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ccc0492c8e58905059cded28cddeeb07
https://ora.ox.ac.uk/objects/uuid:51234d36-f73b-4d10-b4ce-d29b9f9eb7fa
https://ora.ox.ac.uk/objects/uuid:51234d36-f73b-4d10-b4ce-d29b9f9eb7fa
Autor:
R J Graham, J W Steeds
Publikováno v:
Microscopy of Semiconducting Materials, 1983
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2037a819702100cd6ecf73a1bd6c6c49
https://doi.org/10.1201/9781003069614-77
https://doi.org/10.1201/9781003069614-77
Autor:
R. J. Graham, Tiffany A. Shaw
Modern theories of the midlatitude storm tracks connect their intensity to surface baroclinicity (latitudinal surface temperature gradient). However, simulations show storm tracks were weaker during past cold, icy climates relative to the modern clim
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5e82ad813039cad799864979dfb28da3
https://doi.org/10.5194/egusphere-egu2020-2462
https://doi.org/10.5194/egusphere-egu2020-2462
Autor:
Raymond T. Pierrehumbert, R. J. Graham
Publikováno v:
The Astrophysical Journal
The "liquid water habitable zone" (HZ) concept is predicated on the ability of the silicate weathering feedback to stabilize climate across a wide range of instellations. However, representations of silicate weathering used in current estimates of th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9e93515fa00275d4b839473330659b54
According to the Snowball Earth hypothesis, Earth has experienced periods of low-latitude glaciation in its deep past. Prior studies have used general circulation models (GCMs) to examine the effects such an extreme climate state might have on the st
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0eac824a20106ba095d9bd2c2cbdc0f3
Autor:
Predrag Popovic, D. A. Plotkin, J. Checlair, Dorian S. Abbot, R. J. Graham, Jonah Bloch-Johnson, N. X. Farahat, Francisco Spaulding-Astudillo
The ice-albedo feedback on rapidly-rotating terrestrial planets in the habitable zone can lead to abrupt transitions (bifurcations) between a warm and a snowball (ice-covered) state, bistability between these states, and hysteresis in planetary clima
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c072701d875d39fc2fac8804c4cbe97f
http://arxiv.org/abs/1801.10551
http://arxiv.org/abs/1801.10551