標(biāo)題: Titlebook: Coastal and Shelf Sea Modelling; Philip Dyke Book 2001 Springer Science+Business Media New York 2001 Coast.Continental shelf.Ocean.ecosyst [打印本頁(yè)] 作者: 迅速 時(shí)間: 2025-3-21 17:47
書(shū)目名稱Coastal and Shelf Sea Modelling影響因子(影響力)
書(shū)目名稱Coastal and Shelf Sea Modelling影響因子(影響力)學(xué)科排名
書(shū)目名稱Coastal and Shelf Sea Modelling網(wǎng)絡(luò)公開(kāi)度
書(shū)目名稱Coastal and Shelf Sea Modelling網(wǎng)絡(luò)公開(kāi)度學(xué)科排名
書(shū)目名稱Coastal and Shelf Sea Modelling被引頻次
書(shū)目名稱Coastal and Shelf Sea Modelling被引頻次學(xué)科排名
書(shū)目名稱Coastal and Shelf Sea Modelling年度引用
書(shū)目名稱Coastal and Shelf Sea Modelling年度引用學(xué)科排名
書(shū)目名稱Coastal and Shelf Sea Modelling讀者反饋
書(shū)目名稱Coastal and Shelf Sea Modelling讀者反饋學(xué)科排名
作者: 一個(gè)攪動(dòng)不安 時(shí)間: 2025-3-21 23:30
Dynamic Balances, of introduction are appropriate. Many, not to say most variables can be expressed in terms of time (measured in seconds), length (measured in metres) and mass (measured in kilograms). Examples are speed (length divided by time), density (mass divided by volume, hence mass divided by length.) and pr作者: Kinetic 時(shí)間: 2025-3-22 03:30
Numerical Methods,les. However a brief recap is a good idea. For those who are familiar with finite differences the next section should be easy, however there are many environmental scientists without this background so no apology for the brief recap is necessary. Most of the effort should be channeled to understandi作者: 違法事實(shí) 時(shí)間: 2025-3-22 08:16 作者: Delirium 時(shí)間: 2025-3-22 10:56 作者: 破布 時(shí)間: 2025-3-22 15:38
Modelling on the Continental Shelf,, continental shelves. These shelves border the margins of the oceans, the seas over them are only about 200 m deep, and the transition from this 200 m to the oceanic 3000–4000m is achieved through a relatively small region, the continental slope — which is aptly named, since the slope is commonly q作者: 破布 時(shí)間: 2025-3-22 19:38
Environmental Impact Modelling,ome of it is absorbed and some of it is reflected back into space. Surfaces such as the upper surfaces of clouds and snow are particularly efficient at reflection whereas other surfaces such as the sea and forest are not. As the earth is warmed by this radiation, it is emitted back into the atmosphe作者: Gum-Disease 時(shí)間: 2025-3-23 01:13
Modelling in Action,ced in the first seven chapters. Do not worry if you have no expertise in mathematics, or if some of the more technical parts of the book so far have seemed impossible to understand, the whole point of this chapter is to start from the very beginning and to take you through simple models using a ste作者: 熱情的我 時(shí)間: 2025-3-23 04:08 作者: 會(huì)議 時(shí)間: 2025-3-23 09:09 作者: 感激小女 時(shí)間: 2025-3-23 12:53 作者: 都相信我的話 時(shí)間: 2025-3-23 14:27
Dynamic Balances,me scales of many centuries, but something in between. An estuarine modeller would not be concerned with length scales of hundreds or thousands of kilometres but something much less. Most phenomena in ocean science are scale specific due principally to the dominance of the Coriolis effect, and the a作者: Collected 時(shí)間: 2025-3-23 19:47
Modelling Diffusion,ws. Of course this growth is enhanced if there are currents present. The school experiment that demonstrates convection by dropping a crystal of .. (potassium permanganate) in a beaker of water being heated from beneath by a bunsen burner clearly shows enhanced spreading. Similarly in the environmen作者: SAGE 時(shí)間: 2025-3-24 01:51 作者: 規(guī)范要多 時(shí)間: 2025-3-24 06:22 作者: 天氣 時(shí)間: 2025-3-24 08:26 作者: 勉勵(lì) 時(shí)間: 2025-3-24 11:43
Legal aspects and policy issues, of Chapter 2, but suffice it to say that measurements of quantities such as wave height, current speed and direction, the force on pier or jetty can be made on the model. Appropriate scale factors are then applied and an estimate of the real life wave height, current speed and direction, force on t作者: Apogee 時(shí)間: 2025-3-24 15:05
https://doi.org/10.1007/978-1-4899-2969-3me scales of many centuries, but something in between. An estuarine modeller would not be concerned with length scales of hundreds or thousands of kilometres but something much less. Most phenomena in ocean science are scale specific due principally to the dominance of the Coriolis effect, and the a作者: 表否定 時(shí)間: 2025-3-24 21:52 作者: Overstate 時(shí)間: 2025-3-24 23:21
History of the use of seclusion,nificant source and sink of energy for many different types of flow. However, importantly for continental shelf modellers it serves to mark the border between deep ocean and continental shelf, and is the site of the open boundary condition. The dimensions of the continental shelf render models of co作者: Paraplegia 時(shí)間: 2025-3-25 04:14
https://doi.org/10.1007/978-3-319-16006-1e present. The problem now of course that mankind is pumping carbon dioxide and other gases into the atmosphere whilst eliminating large areas of equatorial forest the trees in which provide natural absorbers for these gases. Other effects such as acid rain are also important and are a consequence g作者: 不可侵犯 時(shí)間: 2025-3-25 08:02
Recent Change—Sea Level and Wind Waveswhat I wish to achieve here is a similar easy to follow run through of some of the more elementary but nevertheless instructive marine modelling examples. As the problems are introduced, you are strongly advised to actually stop reading and do the problems . looking at the answer which will appear b作者: ALLEY 時(shí)間: 2025-3-25 14:36 作者: archenemy 時(shí)間: 2025-3-25 19:36 作者: 逃避系列單詞 時(shí)間: 2025-3-25 21:23 作者: Throttle 時(shí)間: 2025-3-26 02:20
History of the use of seclusion,les. However a brief recap is a good idea. For those who are familiar with finite differences the next section should be easy, however there are many environmental scientists without this background so no apology for the brief recap is necessary. Most of the effort should be channeled to understandi作者: Esophagitis 時(shí)間: 2025-3-26 06:07 作者: right-atrium 時(shí)間: 2025-3-26 12:11 作者: 作繭自縛 時(shí)間: 2025-3-26 14:03 作者: Carcinogen 時(shí)間: 2025-3-26 18:04
https://doi.org/10.1007/978-3-319-16006-1ome of it is absorbed and some of it is reflected back into space. Surfaces such as the upper surfaces of clouds and snow are particularly efficient at reflection whereas other surfaces such as the sea and forest are not. As the earth is warmed by this radiation, it is emitted back into the atmosphe作者: 運(yùn)氣 時(shí)間: 2025-3-26 22:09 作者: 吝嗇性 時(shí)間: 2025-3-27 03:12 作者: Excise 時(shí)間: 2025-3-27 08:55 作者: 相反放置 時(shí)間: 2025-3-27 13:02 作者: fatuity 時(shí)間: 2025-3-27 17:25 作者: gangrene 時(shí)間: 2025-3-27 20:31
Boundary Conditions,irms this (see section 3.3 on tidal modelling for example). Therefore the effects that are literally on the edge of models are in fact central drivers and play a major role in determining the resulting motion of the sea.作者: 認(rèn)為 時(shí)間: 2025-3-28 00:31 作者: tic-douloureux 時(shí)間: 2025-3-28 02:32 作者: ODIUM 時(shí)間: 2025-3-28 08:51
Numerical Methods,ng the wider implications of applying the methods and not so much on the fine details. It is accepted that what follows will not perhaps enable the reader to build his or her own model from equations to computer code, it should however help you to understand existing software and more importantly be better able to judge their pitfalls.作者: Compassionate 時(shí)間: 2025-3-28 11:59
Book 2001ses in the sea operate. The coast and thecontinental shelf are two of the most important areas of the sea tounderstand. .Coastal and Shelf Sea Modelling. is therefore verytimely and important. In this text, modelling the processes that occurin the sea is motivated continually through real life examp作者: 說(shuō)明 時(shí)間: 2025-3-28 15:30
10樓作者: THROB 時(shí)間: 2025-3-28 18:47
10樓
