Zobrazeno 1 - 10
of 47
pro vyhledávání: '"Julian Adem"'
Autor:
Yuri N. Skiba, Julian Adem
Publikováno v:
Geofísica Internacional, Vol 34, Iss 4, Pp 385-393 (1995)
Por medio de condiciones especiales de frontera. el problema bien establecido se formula para el modelo oceánico termodinámico de Adem en una región de océano abierta. cuando existe un flujo anómalo de calor a través de las fronteras laterales.
Externí odkaz:
https://doaj.org/article/8272ed7a39d242c595939ce0c6424765
Autor:
Julian Adem
Publikováno v:
Geofísica Internacional, Vol 13, Iss 1, Pp 1-71 (1973)
Un modelo termodinámico se usa, para el hemisferio norte, en enero y en julio, para evaluar en el sistema Atmósfera-Océano-Continente las contribuciones, en los campos de temperatura, de la evaporación y del calor sensible dado a la atmósfera de
Externí odkaz:
https://doaj.org/article/35669d8a3c824fb4867609c28212c29e
Publikováno v:
Advances in Space Research. 57:1373-1390
We use a Thermodynamic Climate Model (TCM) to compute the Northern Hemisphere temperature anomaly for the period 1980–2095, corresponding to the global warming (GW) by the increase of the atmospheric CO2; the GW is in turn diminished as a consequen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f324216614b18cb45d70d8ea42689917
https://doi.org/10.1016/j.asr.2015.11.024
https://doi.org/10.1016/j.asr.2015.11.024
Publikováno v:
Atmospheric Research. 137:228-244
Five composite anomaly fields (CAF) are built for the summer of each Pacific decadal oscillation (PDO) phase: skin temperature; air temperature ( T 7 ), zonal ( u 7 ) and meridional ( v 7 ) wind at the 700 mb level; and precipitation ( R ). An energy
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fc37340d4af0c756b4e767c0b46716c9
https://doi.org/10.1016/j.atmosres.2013.10.010
https://doi.org/10.1016/j.atmosres.2013.10.010
Publikováno v:
Journal of Atmospheric and Solar-Terrestrial Physics. 72:1122-1128
It is uncertain whether the solar cycle 24 will have a high or a low sunspot maximum number. In its last revision the Solar Cycle 24 Prediction Panel indicates that the low prediction is the most likely. Also, solar cycle 25 is considered to present
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a5dd571ec97cf818e963eaf63dd9396a
https://doi.org/10.1016/j.jastp.2010.05.018
https://doi.org/10.1016/j.jastp.2010.05.018
Autor:
V. M. Mendoza, A. S. Mendoza, Julian Adem, René Garduño, Y. Nava, B. Oda, E. E. Villanueva, G. Santisteban
Publikováno v:
International Journal of Climatology. 29:1131-1153
From the climatologic data bases (SICLIM and CLICOM) built by the Servicio Meteorologico Nacional (SMN) of Mexico, we have defined two normals: one called Period I, from 1950 to 1975, and the other called Period II, from 1976 to 2000. The objective o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6655083553605493553907470ec64b73
https://doi.org/10.1002/joc.1728
https://doi.org/10.1002/joc.1728
Publikováno v:
Journal of Atmospheric and Solar-Terrestrial Physics. 66:1683-1690
We have used the thermodynamic model of the climate to estimate the effect of variations in the oceanic cloud cover on the surface temperature of the Earth in the North Hemisphere (NH) during the period 1984–1990. We assume that the variations in t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::90d979b5fedb762162fffb6e04754750
https://doi.org/10.1016/j.jastp.2003.12.003
https://doi.org/10.1016/j.jastp.2003.12.003
Publikováno v:
Journal of Marine Systems. 26:289-302
A thermodynamic model is used to predict the sea surface temperature (SST) anomalies in the Gulf of Mexico for extended periods as long as 3 months and for seasonal prediction. The basic equation of the model is the thermodynamic energy equation appl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e3b10061f6c71194c5e38c036bac76db
https://doi.org/10.1016/s0924-7963(00)00040-3
https://doi.org/10.1016/s0924-7963(00)00040-3
Autor:
Yuri N. Skiba, Julian Adem
Publikováno v:
Numerical Methods for Partial Differential Equations. 14:649-665
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::63f4576187056ee36db94a8a3018233a
https://doi.org/10.1002/(sici)1098-2426(199809)14:5<649::aid-num7>3.0.co
https://doi.org/10.1002/(sici)1098-2426(199809)14:5<649::aid-num7>3.0.co
Publikováno v:
Annales Geophysicae, Vol 16, Pp 853-865 (1998)
Annales Geophysicae, Vol 16, Iss 7, Pp 853-865 (0000)
Annales Geophysicae, Vol 16, Iss 7, Pp 853-865 (0000)
To improve results in monthly rainfall prediction, a parametrization of precipitation has been developed. The thermodynamic energy equation used in the Adem thermodynamic model (ATM) and the Clausius and Clapeyron equation, were used to obtain a line
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1003514fae16e26cca6d47a4f2093d73
https://www.ann-geophys.net/16/853/1998/angeo-16-853-1998.pdf
https://www.ann-geophys.net/16/853/1998/angeo-16-853-1998.pdf