標(biāo)題: Titlebook: Climate and circulation of the tropics; Stefan Hastenrath Book 1985 D. Reidel Publishing Company 1985 climate [打印本頁] 作者: 大口水罐 時間: 2025-3-21 20:07
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作者: Organonitrile 時間: 2025-3-21 22:32
https://doi.org/10.1007/1-4020-5045-3l energetics. Sea-air interaction processes play an important role in this context. Because of the latent heats involved in phase changes, the continuity of water is directly related to that of energy.作者: Gene408 時間: 2025-3-22 01:22
https://doi.org/10.1007/1-4020-5045-3the realm of the subtropical anticyclones of both hemispheres, over the trade wind regimes, to the equatorial trough zone and associated confluence and convergence belts. The focus will be on the atmosphere, although it will on occasion become necessary to refer to the hydrospheric portion of the coupled system.作者: 復(fù)習(xí) 時間: 2025-3-22 07:11
https://doi.org/10.1007/1-4020-5045-3riability of the combined atmosphere-hydrosphere system are manifest in changes of the atmospheric and oceanic circulation and extreme events — especially rainfall anomalies — in the regional climates. Regional climate anomalies appear in part related to circulation changes on the scale of the global tropics.作者: 錯事 時間: 2025-3-22 09:36
The Goal of Artificial Intelligencepressure and other data at distant locations; (iii) the relation between rainfall in the pre-season and at the height of the rainy season; (iv) comprehensive diagnostic studies of climate and circulation anomalies combined with statistical methods; and anticipated for the future (v) numerical modelling.作者: circuit 時間: 2025-3-22 16:15
Climate Prediction,pressure and other data at distant locations; (iii) the relation between rainfall in the pre-season and at the height of the rainy season; (iv) comprehensive diagnostic studies of climate and circulation anomalies combined with statistical methods; and anticipated for the future (v) numerical modelling.作者: circuit 時間: 2025-3-22 18:33
https://doi.org/10.1007/1-4020-5045-3. 1–20; World Meteorological Organization, 1980, pp. 12–15, 38–44; Federal Coordinating Council, 1977, pp. 11, 19–20, 23, 35, 41, 43; National Oceanic and Atmospheric Administration, 1977, pp. 11–13, 17–18, 20–29, 41–45; 1980, pp. 36–68; Department of Commerce, 1980, pp. 8, 13, 24).作者: mastoid-bone 時間: 2025-3-22 21:29 作者: Rustproof 時間: 2025-3-23 03:46
Introduction,. 1–20; World Meteorological Organization, 1980, pp. 12–15, 38–44; Federal Coordinating Council, 1977, pp. 11, 19–20, 23, 35, 41, 43; National Oceanic and Atmospheric Administration, 1977, pp. 11–13, 17–18, 20–29, 41–45; 1980, pp. 36–68; Department of Commerce, 1980, pp. 8, 13, 24).作者: STERN 時間: 2025-3-23 08:03
Planetary Scale Atmospheric Circulation, energy, as discussed in Sections 3.4 and 3.5, involves eddy mechanisms and cannot be accounted for by mean property distributions in meridional-vertical planes. Since kinetic energy amounts only to a small fraction of the total energy content, it is here considered separate from the budgets of heat and moisture addressed in Chapter 5.作者: adulterant 時間: 2025-3-23 10:10
1383-8601 climatic variability in low latitudes, and the associated manifold environmental and societal consequences. Beyond the traditional emphasis of meteor- ology on weather analysis and forecasting, there is a growing interest in the climate and large- scale circulation of the tropics. This book may serv作者: Insul島 時間: 2025-3-23 13:56
Ocean Circulation,f ocean circulation are reviewed here, largely following the presentations in standard texts. However the dynamics of the equatorial ocean in particular are still at the focus of current research and new perspectives are imminent.作者: 完成才會征服 時間: 2025-3-23 18:26 作者: MOAT 時間: 2025-3-23 22:15 作者: 農(nóng)學(xué) 時間: 2025-3-24 05:23
Interannual Variability of the Atmosphere-Ocean System,riability of the combined atmosphere-hydrosphere system are manifest in changes of the atmospheric and oceanic circulation and extreme events — especially rainfall anomalies — in the regional climates. Regional climate anomalies appear in part related to circulation changes on the scale of the global tropics.作者: Trochlea 時間: 2025-3-24 10:13
Book 1985ariability in low latitudes, and the associated manifold environmental and societal consequences. Beyond the traditional emphasis of meteor- ology on weather analysis and forecasting, there is a growing interest in the climate and large- scale circulation of the tropics. This book may serve as a tex作者: FEAT 時間: 2025-3-24 14:37
https://doi.org/10.1007/1-4020-5045-3ales involved in climate processes, investigation of the World ocean is indispensable. It is therefore not surprising that international and national efforts at global climate dynamics have recognized studies of climate mechanisms in low latitudes and of the role of the hydrosphere as tasks of high 作者: FADE 時間: 2025-3-24 18:49 作者: sacrum 時間: 2025-3-24 22:57
https://doi.org/10.1007/1-4020-5045-3nal-vertical cross-sections. Thus the distribution of temperature and humidity is discussed in Section 3.1. The temperature and humidity distribution is, through the thickness pattern and the slope of constant pressure surfaces, related to the zonal wind regime, as reviewed in Section 3.2. The mean 作者: 啪心兒跳動 時間: 2025-3-25 03:00 作者: 有雜色 時間: 2025-3-25 04:08 作者: 最后一個 時間: 2025-3-25 08:24
https://doi.org/10.1007/1-4020-5045-3descending branches of these cells and the associated anticyclonic axes in the lower troposphere provide a natural delineation of the poleward extremities of the tropical atmosphere. Accordingly, the discussion of regional circulation systems in this chapter will in Sections 6.3 to 6.6 proceed from 作者: heterogeneous 時間: 2025-3-25 11:47
https://doi.org/10.1007/1-4020-5045-3s to be concentrated. The purpose of the present chapter is to review the large-scale environmental setting, and the regional and seasonal characteristics of prominent synoptic weather systems. Atmospheric disturbances are individuals rather than identical replicas of each other. Synoptic models are作者: Ganglion 時間: 2025-3-25 17:01 作者: forager 時間: 2025-3-25 21:16
The Goal of Artificial Intelligence0). It is therefore not surprising that endeavors to forecast them well in advance extend over a century, and that both the world Climate Program (World Meteorological Organization, 1980, p. 42) and the U.S. National Climate Program (National Climate Program Office, NOAA, 1980, pp. 23–24) identify c作者: 惹人反感 時間: 2025-3-26 02:25
Rigid Geometry of Curves and Their Jacobiansogical Organization, 1980, pp. 7–10, 28–37; World Meteorological Organization-ICSU, 1975, pp. 1–3; United Nations Environment Programme, 1979, pp. 1–16; National Climate Program Office NOAA, 1980, pp. 1–4, 55–58). There is a two-way interaction between the climatic environment and human activities. 作者: 改革運(yùn)動 時間: 2025-3-26 07:58
Construction of non-kahler 3-folds,ime scale. This final chapter is a preliminary synopsis of climate and circulation conditions in the tropics in the geological past. The available field evidence limits this attempt mainly to the last 30 000 years. For the more distant past refer to the comprehensive review of Crowley (1983).作者: oxidize 時間: 2025-3-26 10:41
978-94-010-8878-7D. Reidel Publishing Company 1985作者: Frisky 時間: 2025-3-26 13:48
Past Climates of the Tropics,ime scale. This final chapter is a preliminary synopsis of climate and circulation conditions in the tropics in the geological past. The available field evidence limits this attempt mainly to the last 30 000 years. For the more distant past refer to the comprehensive review of Crowley (1983).作者: 顯微鏡 時間: 2025-3-26 16:51
Climate and circulation of the tropics978-94-009-5388-8Series ISSN 1383-8601 Series E-ISSN 2215-162X 作者: LVAD360 時間: 2025-3-27 00:55 作者: Overdose 時間: 2025-3-27 02:19
Atmospheric and Oceanographic Sciences Libraryhttp://image.papertrans.cn/c/image/227672.jpg作者: gimmick 時間: 2025-3-27 07:06 作者: 清晰 時間: 2025-3-27 09:54
Diurnal Forcings and Local Circulations, latitudes where the diurnal is much smaller than the annual cycle. Forcings on the time scale of a day or less result from horizontal contrasts in the surface heat budget and thermal and gravitational atmospheric tides; both heat budget and tidal forcings being particularly pronounced in the low la作者: 譏諷 時間: 2025-3-27 13:45
Planetary Scale Atmospheric Circulation,nal-vertical cross-sections. Thus the distribution of temperature and humidity is discussed in Section 3.1. The temperature and humidity distribution is, through the thickness pattern and the slope of constant pressure surfaces, related to the zonal wind regime, as reviewed in Section 3.2. The mean 作者: 放大 時間: 2025-3-27 18:49
Ocean Circulation,budget (Chapter 5), in the quasi-permanent circulation systems of the lower atmosphere (Chapter 6), in the mechanisms of interannual variability and regional climate anomalies (Chapters 8–9), and in the characteristics of past climates (Chapters 11–12). As a background for these topics, the basics o作者: grenade 時間: 2025-3-28 00:02 作者: plasma 時間: 2025-3-28 03:11
Regional Circulation Systems,descending branches of these cells and the associated anticyclonic axes in the lower troposphere provide a natural delineation of the poleward extremities of the tropical atmosphere. Accordingly, the discussion of regional circulation systems in this chapter will in Sections 6.3 to 6.6 proceed from 作者: 性學(xué)院 時間: 2025-3-28 07:43
Climatology of Weather Systems,s to be concentrated. The purpose of the present chapter is to review the large-scale environmental setting, and the regional and seasonal characteristics of prominent synoptic weather systems. Atmospheric disturbances are individuals rather than identical replicas of each other. Synoptic models are作者: 偏狂癥 時間: 2025-3-28 10:34
Interannual Variability of the Atmosphere-Ocean System,ssed in Chapters 6 and 7, while Chapter 4 provides an orientation on the characteristic average mode of operation of the low-latitude oceans. This background is required for the understanding of year-to-year variations which are to be explored in the present chapter. The mechanisms of interannual va作者: Carcinoma 時間: 2025-3-28 18:14 作者: 音的強(qiáng)弱 時間: 2025-3-28 22:49 作者: Obligatory 時間: 2025-3-29 02:11
Past Climates of the Tropics,ime scale. This final chapter is a preliminary synopsis of climate and circulation conditions in the tropics in the geological past. The available field evidence limits this attempt mainly to the last 30 000 years. For the more distant past refer to the comprehensive review of Crowley (1983).作者: 會犯錯誤 時間: 2025-3-29 05:45
Diurnal Forcings and Local Circulations,oning of the tropical atmosphere does not seem to have received the attention it deserves. The present chapter is intended as a preliminary review of such diurnal and local processes, and as reference for subjects discussed in later chapters of this book.
