作者: 吸引人的花招 時(shí)間: 2025-3-21 23:33 作者: 駭人 時(shí)間: 2025-3-22 03:03
Can Box Ocean Models Calibrated by Inverse Methods Provide a Means of Testing Ocean Circulation Modesting ocean circulation models is elucidated with examples comparing a global 12-box model (Bolin .., 1983) and an Atlantic 84-box model (Bolin .., 1987). It is found that steady-state chemical tracers provide constraints only on the largest (basin-wide) scales. Arguments are presented for developin作者: 陰謀小團(tuán)體 時(shí)間: 2025-3-22 08:02
General Circulation Modelling of the Atmospheres of the Meteorological Office AGCM are presented and assessed against climatological data. Examples are given of the changes in surface fluxes in numerical experiments with CO.. Finally, the problems of coupling atmosphere and ocean models are discussed and future advances in atmospheric modelling 作者: Stable-Angina 時(shí)間: 2025-3-22 10:56
An Ocean Modelling System for Supercomputer Architectures of the 1990s in computer technology offer considerable promise for changing this situation—if judicious use is made of supercomputers. In order to realize the desired goal of being able to simulate global ocean circulation with resolved eddies within “reasonable” time constraints, a model has been developed to 作者: Agility 時(shí)間: 2025-3-22 16:41 作者: Agility 時(shí)間: 2025-3-22 17:25
ENSO Modelling at MPIn Oscillation (ENSO) phenomenon are briefly reviewed. The studies described encompass the investigation of the atmospheric response to observed sea surface temperatures (SSTs), the oceanic response to observed wind stresses, and studies with coupled ocean-atmosphere models investigating large-scale 作者: 連累 時(shí)間: 2025-3-23 01:11
Specification and Variability of the Surface Forcing of the Oceands of providing the non-interactive forcing for ocean circulation models are reviewed and the sensitivities of a model of the tropical Pacific to the use of forcing datasets derived from observed climatology and from an atmospheric general circulation model are described, together with the sensitivi作者: 小故事 時(shí)間: 2025-3-23 03:36
Modelling of Geochemical Tracers in the Oceanonal current field of an OGCM. The modelled tracers are phosphate, alkalinity, oxygen, dissolved inorganic carbon, particulate organic carbon, and calcite, the latter three in three isotopes. By an appropriate choice of inventories and metabolic rates, a satisfactory agreement with data, especially 作者: 使增至最大 時(shí)間: 2025-3-23 05:38 作者: Ondines-curse 時(shí)間: 2025-3-23 10:37
Climatic Change and Ocean Bottom Water Formation: Are We Missing Something?pwelling over all the world’s oceans. Relatively shallow, thermally-driven convective overturning occurring at high latitudes which arises from heating of the atmosphere by the oceans is fairly well represented in current numerical ocean models, but deep convection from surface salinity sources incl作者: seroma 時(shí)間: 2025-3-23 15:31
,Das natürliche elektromagnetische Umfeld,ttention is primarily given to the annual-mean fields which are of significance for long-term trends in climate, although aspects of the seasonal variations contributing to these are presented where relevant. Preliminary results from a coupled atmosphere/ocean/sea-ice model are discussed in terms of作者: Leaven 時(shí)間: 2025-3-23 19:26 作者: 北極人 時(shí)間: 2025-3-24 00:54 作者: 人造 時(shí)間: 2025-3-24 04:24 作者: 哥哥噴涌而出 時(shí)間: 2025-3-24 07:33 作者: 準(zhǔn)則 時(shí)間: 2025-3-24 13:41 作者: 軍械庫(kù) 時(shí)間: 2025-3-24 16:47
Sicherheitsversprechen im Wandeln Oscillation (ENSO) phenomenon are briefly reviewed. The studies described encompass the investigation of the atmospheric response to observed sea surface temperatures (SSTs), the oceanic response to observed wind stresses, and studies with coupled ocean-atmosphere models investigating large-scale 作者: 冰河期 時(shí)間: 2025-3-24 19:30
Rolf Arnold,Marcel Berg,Horst Müller-Petersds of providing the non-interactive forcing for ocean circulation models are reviewed and the sensitivities of a model of the tropical Pacific to the use of forcing datasets derived from observed climatology and from an atmospheric general circulation model are described, together with the sensitivi作者: 新手 時(shí)間: 2025-3-25 02:36
Risikokompetenz und deren Hemmnisseonal current field of an OGCM. The modelled tracers are phosphate, alkalinity, oxygen, dissolved inorganic carbon, particulate organic carbon, and calcite, the latter three in three isotopes. By an appropriate choice of inventories and metabolic rates, a satisfactory agreement with data, especially 作者: 光明正大 時(shí)間: 2025-3-25 03:54 作者: 我沒(méi)有命令 時(shí)間: 2025-3-25 09:28 作者: 首創(chuàng)精神 時(shí)間: 2025-3-25 11:48
https://doi.org/10.1007/978-94-009-2093-4Ocean; Scale; Sea ice; satellite; temperature作者: 善于騙人 時(shí)間: 2025-3-25 18:10 作者: plasma 時(shí)間: 2025-3-25 22:07
,Risiko Gesundheit. Eine Einführung,s of the Meteorological Office AGCM are presented and assessed against climatological data. Examples are given of the changes in surface fluxes in numerical experiments with CO.. Finally, the problems of coupling atmosphere and ocean models are discussed and future advances in atmospheric modelling are considered.作者: NICE 時(shí)間: 2025-3-26 01:56 作者: 聽(tīng)寫 時(shí)間: 2025-3-26 06:24
Risikokompetenz und deren Hemmnisseonal current field of an OGCM. The modelled tracers are phosphate, alkalinity, oxygen, dissolved inorganic carbon, particulate organic carbon, and calcite, the latter three in three isotopes. By an appropriate choice of inventories and metabolic rates, a satisfactory agreement with data, especially the GEOSECS data, could be achieved.作者: 玷污 時(shí)間: 2025-3-26 10:39 作者: 思想靈活 時(shí)間: 2025-3-26 12:42
http://image.papertrans.cn/c/image/227690.jpg作者: uncertain 時(shí)間: 2025-3-26 18:44 作者: 本能 時(shí)間: 2025-3-26 21:08
Extratropical Response to SST Anomalies and the Barotropic ModelRecent GCM integrations with El Ni?o sea surface temperature anomalies are reviewed, and the question of whether the extratropical response can be explained in terms of simple barotropic model dynamics is examined.作者: 盤旋 時(shí)間: 2025-3-27 01:57
General Circulation Modelling of the Atmospheres of the Meteorological Office AGCM are presented and assessed against climatological data. Examples are given of the changes in surface fluxes in numerical experiments with CO.. Finally, the problems of coupling atmosphere and ocean models are discussed and future advances in atmospheric modelling are considered.作者: Kindle 時(shí)間: 2025-3-27 05:18 作者: Little 時(shí)間: 2025-3-27 10:37
Modelling of Geochemical Tracers in the Oceanonal current field of an OGCM. The modelled tracers are phosphate, alkalinity, oxygen, dissolved inorganic carbon, particulate organic carbon, and calcite, the latter three in three isotopes. By an appropriate choice of inventories and metabolic rates, a satisfactory agreement with data, especially the GEOSECS data, could be achieved.作者: GORGE 時(shí)間: 2025-3-27 16:34 作者: Silent-Ischemia 時(shí)間: 2025-3-27 18:04 作者: 神經(jīng) 時(shí)間: 2025-3-28 01:13
,Das natürliche elektromagnetische Umfeld,ations contributing to these are presented where relevant. Preliminary results from a coupled atmosphere/ocean/sea-ice model are discussed in terms of the differences between the transports in the ocean model and those observed.作者: Agnosia 時(shí)間: 2025-3-28 05:13 作者: 收養(yǎng) 時(shí)間: 2025-3-28 07:28
Rolf Arnold,Marcel Berg,Horst Müller-Petersuse of forcing datasets derived from observed climatology and from an atmospheric general circulation model are described, together with the sensitivity of the sea surface temperature simulation in a coupled atmosphere-ocean model to inclusion of a simple representation of subgrid-scale motions associated with regions of deep convection.作者: Flounder 時(shí)間: 2025-3-28 11:24 作者: 吃掉 時(shí)間: 2025-3-28 15:53 作者: 怒目而視 時(shí)間: 2025-3-28 19:25
Specification and Variability of the Surface Forcing of the Oceanuse of forcing datasets derived from observed climatology and from an atmospheric general circulation model are described, together with the sensitivity of the sea surface temperature simulation in a coupled atmosphere-ocean model to inclusion of a simple representation of subgrid-scale motions associated with regions of deep convection.作者: 不溶解 時(shí)間: 2025-3-29 01:11 作者: Introduction 時(shí)間: 2025-3-29 06:09
https://doi.org/10.1007/978-3-642-55547-3ncy level. A surprisingly realistic simulation in terms of mean fields and eddy variability was also achieved. Applications with higher resolution using more processors eagerly await future supercomputers.作者: 空氣 時(shí)間: 2025-3-29 07:19
An Ocean Modelling System for Supercomputer Architectures of the 1990sncy level. A surprisingly realistic simulation in terms of mean fields and eddy variability was also achieved. Applications with higher resolution using more processors eagerly await future supercomputers.作者: Terminal 時(shí)間: 2025-3-29 12:23 作者: 放棄 時(shí)間: 2025-3-29 15:46 作者: 遷移 時(shí)間: 2025-3-29 23:20 作者: Conserve 時(shí)間: 2025-3-29 23:56 作者: 思鄉(xiāng)病 時(shí)間: 2025-3-30 06:10 作者: PRE 時(shí)間: 2025-3-30 10:05
https://doi.org/10.1007/978-3-662-46888-3ure anomaly fields in four recent decades are provided, and likely future improvements to this new analysis are outlined. The combined analyses are now making it possible to compare comprehensively changes in global and regional surface temperature observed in recent decades with numerical predictio作者: Osteons 時(shí)間: 2025-3-30 14:49 作者: Fester 時(shí)間: 2025-3-30 17:10
Risikokompetenz und deren Hemmnissetential density increment in the Southern Ocean are in reasonable accord with observations. When the amount of sea ice freezing is expressed as a function of hemispheric mean sea surface temperature (calibrated from the seasonal cycle), the model predicts the possible cutoff of AABW and most of the 作者: 一回合 時(shí)間: 2025-3-30 21:32
Book 1990es of Decades to Centuries, and Impact of Paleoclimatic Proxy Data on Climate Modelling. Preface ix Acknowledgements I thank Howard Cattle and Neil Wells for their guidance and assistance as members of the Workshop Organizing Committee. I particularly thank Michael Davey for all his efforts as Local
