標(biāo)題: Titlebook: Climatic Variations and Variability: Facts and Theories; NATO Advanced Study A. Berger Book 1981 D. Reidel Publishing Company, Dordrecht, [打印本頁(yè)] 作者: 評(píng)估 時(shí)間: 2025-3-21 18:39
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書目名稱Climatic Variations and Variability: Facts and Theories讀者反饋學(xué)科排名
作者: Pudendal-Nerve 時(shí)間: 2025-3-21 23:33 作者: 合唱團(tuán) 時(shí)間: 2025-3-22 00:27
The Memory of the Oceanally. The memory of the smaller motions, the oceanic analogue of weather, is estimated to be a few months according to Lorenz’s (1) criterion based on error growth in numerical models. Such error growth may also limit forecasts of changes in the large scale ocean circulation responding to changes in作者: overhaul 時(shí)間: 2025-3-22 07:29 作者: 躲債 時(shí)間: 2025-3-22 11:44
Glacial to Interglacial Changes in Ocean and Atmosphere Chemistryreenland and Antarctica. A hypothesis for this increase involves the loss of phosphorous from the sea to the shelf sediments during the early postglacial transgression of sea level, reducing the amount of plant matter formed per unit of upwelled water and thereby increasing the CO. pressure in surfa作者: Ophthalmoscope 時(shí)間: 2025-3-22 14:04
Transfer Functions: Calibrating Micropaleontological Data in Climatic Termsare calibrated on a set of geographically-distributed observations which record both the modern climate and the biotic response to climate as reflected in paleontological samples. The technique has been used on tree rings (27) and pollen as well as on planktonic microfossils (including foraminifera,作者: Ophthalmoscope 時(shí)間: 2025-3-22 20:38 作者: Vasoconstrictor 時(shí)間: 2025-3-22 23:13 作者: GRUEL 時(shí)間: 2025-3-23 04:31 作者: 異端邪說(shuō)2 時(shí)間: 2025-3-23 07:07
https://doi.org/10.1007/978-3-642-41048-2d. Non-seasonal tropical free air temperature changes are related to preceeding changes in tropical sea surface temperature and to volcanic aerosol while the tropical sea surface temperature itself is related to changes in surface pressure which characterize the Southern Oscillation. Zonal wind vari作者: heterogeneous 時(shí)間: 2025-3-23 09:56
https://doi.org/10.1007/978-3-642-41048-2ally. The memory of the smaller motions, the oceanic analogue of weather, is estimated to be a few months according to Lorenz’s (1) criterion based on error growth in numerical models. Such error growth may also limit forecasts of changes in the large scale ocean circulation responding to changes in作者: 冥界三河 時(shí)間: 2025-3-23 13:50
Versicherung gegen Fehlerfolgen, computations of the earth heat balance. The albedo of natural surfaces varies with, among others, angular distribution and spectral composition of the incident radiation and with the surface moisture. This makes the determinations of reliable time averaged surface albedo values difficult. Existing 作者: GONG 時(shí)間: 2025-3-23 20:42
,?rztliche ?Behandlungsfehler“,reenland and Antarctica. A hypothesis for this increase involves the loss of phosphorous from the sea to the shelf sediments during the early postglacial transgression of sea level, reducing the amount of plant matter formed per unit of upwelled water and thereby increasing the CO. pressure in surfa作者: 思考才皺眉 時(shí)間: 2025-3-24 01:02
Rechtliche Aspekte von Kunstfehlern,are calibrated on a set of geographically-distributed observations which record both the modern climate and the biotic response to climate as reflected in paleontological samples. The technique has been used on tree rings (27) and pollen as well as on planktonic microfossils (including foraminifera,作者: corn732 時(shí)間: 2025-3-24 04:20 作者: 大喘氣 時(shí)間: 2025-3-24 07:49
,Team-Time-Out – bevor es zu sp?t ist,hile the archived data are generally available for those who need them, there will be many of the same kinds of climate-related data that are not so generally available; but steps are being taken under the World Climate Programme to improve this situation.作者: Cpap155 時(shí)間: 2025-3-24 10:54 作者: fulcrum 時(shí)間: 2025-3-24 17:25
Data Banks for Climatological Purposeshile the archived data are generally available for those who need them, there will be many of the same kinds of climate-related data that are not so generally available; but steps are being taken under the World Climate Programme to improve this situation.作者: membrane 時(shí)間: 2025-3-24 21:03 作者: 刺耳 時(shí)間: 2025-3-25 02:26
,Team-Time-Out – bevor es zu sp?t ist,hile the archived data are generally available for those who need them, there will be many of the same kinds of climate-related data that are not so generally available; but steps are being taken under the World Climate Programme to improve this situation.作者: 身心疲憊 時(shí)間: 2025-3-25 07:23 作者: Acetaminophen 時(shí)間: 2025-3-25 09:07 作者: 小隔間 時(shí)間: 2025-3-25 15:20 作者: 輕快走過(guò) 時(shí)間: 2025-3-25 19:22 作者: Mettle 時(shí)間: 2025-3-25 21:16 作者: adulterant 時(shí)間: 2025-3-26 02:15 作者: 高深莫測(cè) 時(shí)間: 2025-3-26 05:41
Glacial to Interglacial Changes in Ocean and Atmosphere Chemistryce water and the atmosphere. Evidence in support of this hypothesis is obtained from the .C results for benthic and planktonic foraminifera. Changes in the difference between warm surface water and mean oceanic .C values reflect changes in the oceanic PO. to ΣCO. ratio.作者: 輕信 時(shí)間: 2025-3-26 09:45
https://doi.org/10.1007/978-3-642-41048-2reenland seesaw”. The injection of volcanic aerosol by the eruption of Mt. Agung in March 1963 into the stratosphere gives rise to temperature increases of up to 5°C in the stratosphere and cooling of 1°C in the troposphere. The third major climatic signal in the recent record—the so called “Biennial oscillation”is also briefly reviewed.作者: Urologist 時(shí)間: 2025-3-26 15:37
Rechtliche Aspekte von Kunstfehlern,sonal temperatures and salinity. When applied to samples from a chronostratigraphic horizon, transfer functions yield synoptic charts of past climates. In this form paleontological data are readily interpretable by meteorologists and physical oceanographers, and can be entered as boundary conditions into numerical models of climate.作者: 凹室 時(shí)間: 2025-3-26 20:05
Climatic Changes and Variations: A Geophysical Problemreenland seesaw”. The injection of volcanic aerosol by the eruption of Mt. Agung in March 1963 into the stratosphere gives rise to temperature increases of up to 5°C in the stratosphere and cooling of 1°C in the troposphere. The third major climatic signal in the recent record—the so called “Biennial oscillation”is also briefly reviewed.作者: Nmda-Receptor 時(shí)間: 2025-3-26 21:01
Transfer Functions: Calibrating Micropaleontological Data in Climatic Termssonal temperatures and salinity. When applied to samples from a chronostratigraphic horizon, transfer functions yield synoptic charts of past climates. In this form paleontological data are readily interpretable by meteorologists and physical oceanographers, and can be entered as boundary conditions into numerical models of climate.作者: Ptosis 時(shí)間: 2025-3-27 01:07
1389-2185 at Erice in 1963 by prof. Nino Zichichi, pursues the fundamental aim to create in Europe a cultural forum of high scientific standard, which can allow young research workers to appreciate current problems of major interest in the various fields of scientific research. , Since the beginning, its Int作者: pantomime 時(shí)間: 2025-3-27 09:04 作者: Interstellar 時(shí)間: 2025-3-27 11:05
Surface Albedoe incident radiation and with the surface moisture. This makes the determinations of reliable time averaged surface albedo values difficult. Existing data are inadequate and incomplete. World-wide monitoring of surface albedo variations is long overdue.作者: 來(lái)就得意 時(shí)間: 2025-3-27 13:47 作者: rheumatology 時(shí)間: 2025-3-27 21:10 作者: Triglyceride 時(shí)間: 2025-3-27 22:08 作者: aggrieve 時(shí)間: 2025-3-28 02:43 作者: 恃強(qiáng)凌弱 時(shí)間: 2025-3-28 06:15
Beispiele umgesetzter Ma?nahmen aus CIRSevaluated. In terms of the average sea-level pressure and precipitation such models simulate the observed statistics reasonably well, although a number of modeling problems remain; chief among these is the coupling of the atmosphere and ocean in order to examine the predictability of the climate on 作者: Terminal 時(shí)間: 2025-3-28 13:41
