全球變暖之-氣候模型(雙語)
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KEYWORDS:全球變暖 全球變暖之-氣候模型(雙語) 聲明:本文圖片內(nèi)容來自與互聯(lián)網(wǎng)絡(luò),旨在調(diào)節(jié)視覺疲勞,如有版權(quán)問題,請(qǐng)致電告知。本文英文閱讀文本內(nèi)容來自于國外英文門戶以及資訊資料網(wǎng)站,可能有超語法類的常用正確表達(dá),請(qǐng)大家仔細(xì)審閱,注意甄別。 全球變暖指的是在一段時(shí)間中,地球的大氣和海洋溫度上升的現(xiàn)象,主要是指人為因素造成的溫度上升。原因很可能是由于溫室氣體排放過多造成。 The main tools for projecting future climate changes are mathematical models based on physical principles including fluid dynamics, thermodynamics and radiative transfer. Although they attempt to include as many processes as possible, simplifications of the actual climate system are inevitable because of the constraints of available computer power and limitations in knowledge of the climate system. All modern climate models are in fact combinations of models for different parts of the Earth. These include an atmospheric model for air movement, temperature, clouds, and other atmospheric properties; an ocean model that predicts temperature, salt content, and circulation of ocean waters; models for ice cover on land and sea; and a model of heat and moisture transfer from soil and vegetation to the atmosphere. Some models also include treatments of chemical and biological processes.Warming due to increasing levels of greenhouse gases is not an assumption of the models; rather, it is an end result from the interaction of greenhouse gases with radiative transfer and other physical processes in the models.Although much of the variation in model outcomes depends on the greenhouse gas emissions used as inputs, the temperature effect of a specific greenhouse gas concentration (climate sensitivity) varies depending on the model used. The representation of clouds is one of the main sources of uncertainty in present-generation models. Global climate model projections of future climate most often have used estimates of greenhouse gas emissions from the IPCC Special Report on Emissions Scenarios (SRES). In addition to human-caused emissions, some models also include a simulation of the carbon cycle; this generally shows a positive feedback, though this response is uncertain. Some observational studies also show a positive feedback.Including uncertainties in future greenhouse gas concentrations and climate sensitivity, the IPCC anticipates a warming of 1.1 °C to 6.4 °C (2.0 °F to 11.5 °F) by the end of the 21st century, relative to 1980–1999. Models are also used to help investigate the causes of recent climate change by comparing the observed changes to those that the models project from various natural and human-derived causes. Although these models do not unambiguously attribute the warming that occurred from approximately 1910 to 1945 to either natural variation or human effects, they do indicate that the warming since 1970 is dominated by man-made greenhouse gas emissions. The physical realism of models is tested by examining their ability to simulate current or past climates.Current climate models produce a good match to observations of global temperature changes over the last century, but do not simulate all aspects of climate.Not all effects of global warming are accurately predicted by the climate models used by the IPCC. For example, observed Arctic shrinkage has been faster than that predicted. |
課程名稱 | 老師 | 課時(shí) | 試聽 | 報(bào)名 | 學(xué)費(fèi) |
---|---|---|---|---|---|
托福強(qiáng)化口語班 | 劉志云 | 20 | 試聽 | 報(bào)名 | 200元 |
托福強(qiáng)化閱讀班 | 祁連山 | 18 | 試聽 | 報(bào)名 | 200元 |
托福強(qiáng)化聽力班 | 張 艷 | 44 | 試聽 | 報(bào)名 | 200元 |
托福強(qiáng)化寫作班 | 齊 轍 | 16 | 試聽 | 報(bào)名 | 200元 |
托福基礎(chǔ)聽說班 | 薛涵予 | 25 | 試聽 | 報(bào)名 | 200元 |
托;A(chǔ)閱讀班 | 劉 偉 | 26 | 試聽 | 報(bào)名 | 200元 |
托;A(chǔ)寫作班 | 劉家瑋 | 20 | 試聽 | 報(bào)名 | 200元 |
托福詞匯必備班 | 白 楊 | 19 | 試聽 | 報(bào)名 | 200元 |
熱門資料下載: |
新托?荚囌搲療豳N: |
【責(zé)任編輯:育路編輯 糾錯(cuò)】 |
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閱讀上一篇:全球變暖百科詳述:溫室氣體 |
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閱讀下一篇:全球變暖百科詳述:地表溫度變化 |
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報(bào)考直通車 |
·新托福最近考試時(shí)間:2010年6月26日。 |
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·考試內(nèi)容:閱讀、 聽力、口語、寫作。 |
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