標(biāo)題: Titlebook: Atmospheric Ozone as a Climate Gas; General Circulation Wei-Chyung Wang,Ivar S. A. Isaksen Conference proceedings 1995 Springer-Verlag Ber [打印本頁] 作者: FLAW 時(shí)間: 2025-3-21 18:40
書目名稱Atmospheric Ozone as a Climate Gas影響因子(影響力)
書目名稱Atmospheric Ozone as a Climate Gas影響因子(影響力)學(xué)科排名
書目名稱Atmospheric Ozone as a Climate Gas網(wǎng)絡(luò)公開度
書目名稱Atmospheric Ozone as a Climate Gas網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Atmospheric Ozone as a Climate Gas被引頻次
書目名稱Atmospheric Ozone as a Climate Gas被引頻次學(xué)科排名
書目名稱Atmospheric Ozone as a Climate Gas年度引用
書目名稱Atmospheric Ozone as a Climate Gas年度引用學(xué)科排名
書目名稱Atmospheric Ozone as a Climate Gas讀者反饋
書目名稱Atmospheric Ozone as a Climate Gas讀者反饋學(xué)科排名
作者: keloid 時(shí)間: 2025-3-21 22:58
Climate Modelingtool that can give a first estimate of the possible importance of those changes, while a more detailed understanding may be obtained from experiments using general circulation models (GCMs). These models can be used for sensitivity studies of the climatic response to prescribed ozone changes, howeve作者: Glucose 時(shí)間: 2025-3-22 01:50
Issues Relevant to the Development of Coupled Chemistry/Climate Modelsur decades. In the past, this belief has led to the development of two separate efforts: to understand and build models to describing the physical climate system and to understand and build models of the chemical climate system. But how will these two systems interact? Are there important chemical c作者: 向外供接觸 時(shí)間: 2025-3-22 07:35 作者: Axillary 時(shí)間: 2025-3-22 11:41 作者: HALL 時(shí)間: 2025-3-22 14:39 作者: 艦旗 時(shí)間: 2025-3-22 18:01
Analysis of 25 years of regular ozone soundings at Uccle (Belgium)und statistically significant trends in tropospheric ozone are found that vary between approximately 1.6% near the surface and 1% per year above the mixed layer. Year-round negative ozone trends are found above 18 km and at the level of the secondary ozone maximum in the lower stratosphere during la作者: 性滿足 時(shí)間: 2025-3-23 00:07
Concurrent Ozone and Temperature Trends Derived from Ozonesonde Stationsonde stations, 11 of which are in the Northern Hemisphere. The regression analysis takes into account the seasonal, solar and quasi biennial cycles, plus events like volcanic eruptions and instrument change. For all stations, a significant negative ozone trend in (some regions of) the stratosphere i作者: Hearten 時(shí)間: 2025-3-23 02:52 作者: forager 時(shí)間: 2025-3-23 07:32 作者: 慌張 時(shí)間: 2025-3-23 12:50 作者: 創(chuàng)新 時(shí)間: 2025-3-23 17:37
Radiative Forcing by Tropospheric Ozone Changes due to Increased Emissions of CH4, CO and NOxor (CH., CO, NO.) emissions and to calculate the associated radiative forcing on the climate system. Significant perturbations of tropospheric ozone photochemical produetion and consequently of ozone concentrations are calculated, with important seasonal and latitudinal dependences. For all simulati作者: dandruff 時(shí)間: 2025-3-23 19:23
The Role of Convection in the Vertical Distribution of Ozone and Precursors in the Troposphereconnection with convective clouds and frontal circulation is about 0.6 TgN/yr, and in addition about the same amount of other NO. compounds is injected. For comparison, the various sources at the ground total 34 TgN/yr of NO.. The strength of the lightning source was assumed to be 3 TgN/yr. The tota作者: 滔滔不絕地說 時(shí)間: 2025-3-24 00:37 作者: incisive 時(shí)間: 2025-3-24 02:34
Ozone Chemistry Changes in the Troposphere and Consequent Radiative Forcing of Climatephere since pre-industrial times. Calculated increases of tropospheric O. have been evaluated with a radiative transfer model. Our calculations confirm earlier studies that the combined effects of anthropogenic NO., CO and CH. emissions cause a strong enhancement of O. levels throughout the global t作者: 前面 時(shí)間: 2025-3-24 07:42
A GCM Study of the Climatic Effect of 1979–1992 Ozone TrendM). The GCM employs a newly constructed ozone climatology that includes longitudinal Variation. In the perturbed Simulation, the O. trend is assumed to be confined to the lower stratosphere, and imposed in transient from January 1979 to December 1992 to incorporate both seasonal variations and linea作者: 遺產(chǎn) 時(shí)間: 2025-3-24 13:17
S?tze von Bloch, Picard und Schottkyer stratospheric ozone. There has been statistically significant increases in free tropospheric ozone concentration in some areas of the northem hemisphere and, at the same time, a global decrease in lower stratospheric ozone concentration. The total ozone continues to decline by an average rate of 作者: 代理人 時(shí)間: 2025-3-24 16:57 作者: 陳舊 時(shí)間: 2025-3-24 22:19 作者: cancellous-bone 時(shí)間: 2025-3-25 01:09
Unendliche Produkte holomorpher Funktionentraviolet radiation and outgoing infrared radiation. It also indirectly affects climate because it is intimately linked with the concentration of OH in the troposphere, which ultimately determines the fate of many trace gases (including greenhouse gases). In this paper, we illustrate how climate-rel作者: tariff 時(shí)間: 2025-3-25 04:09 作者: sperse 時(shí)間: 2025-3-25 07:56 作者: nocturia 時(shí)間: 2025-3-25 12:29
Bestimmte Integrale und Residuenkalkülund statistically significant trends in tropospheric ozone are found that vary between approximately 1.6% near the surface and 1% per year above the mixed layer. Year-round negative ozone trends are found above 18 km and at the level of the secondary ozone maximum in the lower stratosphere during la作者: insular 時(shí)間: 2025-3-25 16:14 作者: 代理人 時(shí)間: 2025-3-25 23:29
Laurentreihen und Fourierreihenpheric ozone depletion and ii) increased temperatures and water vapour densities that follow from increased levels of greenhouse gases. Increased UV radiation increases the photolysis rates for several tropospheric gases, in particular ozone. This leads to enhanced levels of odd hydrogen and reduced作者: Common-Migraine 時(shí)間: 2025-3-26 01:58 作者: reaching 時(shí)間: 2025-3-26 05:00
Cauchysche Integralformel und Folgerungen, of 1988. Trajectories are calculated for a case study and the ozone flux during a stratospheric intrusion into the troposphere is calculated to be in the order of 10. molecules/day for a mid-latitude winter cyclone. The occurrence of tropopause folds is linked to long term meteorological trends and作者: deriver 時(shí)間: 2025-3-26 12:27 作者: LAVA 時(shí)間: 2025-3-26 15:58
Funktionentheorie erkunden mit Maple?connection with convective clouds and frontal circulation is about 0.6 TgN/yr, and in addition about the same amount of other NO. compounds is injected. For comparison, the various sources at the ground total 34 TgN/yr of NO.. The strength of the lightning source was assumed to be 3 TgN/yr. The tota作者: Detonate 時(shí)間: 2025-3-26 20:17 作者: DEMUR 時(shí)間: 2025-3-26 21:55
https://doi.org/10.1007/3-7643-7430-6phere since pre-industrial times. Calculated increases of tropospheric O. have been evaluated with a radiative transfer model. Our calculations confirm earlier studies that the combined effects of anthropogenic NO., CO and CH. emissions cause a strong enhancement of O. levels throughout the global t作者: 左右連貫 時(shí)間: 2025-3-27 02:45 作者: dandruff 時(shí)間: 2025-3-27 05:35
Unendliche Produkte holomorpher FunktionenThe abundance of ozone in the upper troposphere and lower stratosphere is governed by photochemical as well as transport processes.作者: 帳單 時(shí)間: 2025-3-27 11:19 作者: Ophthalmologist 時(shí)間: 2025-3-27 14:03 作者: 血友病 時(shí)間: 2025-3-27 21:33
Reinhold Remmert,Georg Schumacherations the models are able to reproduce the main features of the stratospheric dynamics and trace species distributions. As an illustration some results from the models developed at the CNRM are described. The methodology for an interactive coupling between general circulation models and chemical transport models is discussed.作者: 政府 時(shí)間: 2025-3-28 01:49
https://doi.org/10.1007/978-3-642-79869-6Atmosph?re, Chemie der; Klimatologie; Ozon; Ozone; Treibhausgase; Troposphere; atmospheric chemistry; clima作者: Critical 時(shí)間: 2025-3-28 05:02
978-3-642-79871-9Springer-Verlag Berlin Heidelberg 1995作者: 其他 時(shí)間: 2025-3-28 08:15
Nato ASI Subseries I:http://image.papertrans.cn/b/image/164634.jpg作者: 漫不經(jīng)心 時(shí)間: 2025-3-28 10:33
GCM Modeling of the Stratospheric Dynamics and its Coupling with Chemistryations the models are able to reproduce the main features of the stratospheric dynamics and trace species distributions. As an illustration some results from the models developed at the CNRM are described. The methodology for an interactive coupling between general circulation models and chemical transport models is discussed.作者: 大炮 時(shí)間: 2025-3-28 18:06 作者: octogenarian 時(shí)間: 2025-3-28 19:10
Upper Tropospheric/Lower Stratospheric Ozone Climatologyion in Australia and one in Brazil, however with periods with a measurement frequency less than one sonde per week. In general, the data quality is uneven between these stations. If a better assessment is to be made of ozone impaets on climate, research must establish the trend in ozone concentratio作者: Self-Help-Group 時(shí)間: 2025-3-28 23:02 作者: 痛得哭了 時(shí)間: 2025-3-29 03:41
Simulations of Stratospheric Ozone in a Climate Modelhe 42 level model. In contrast, the 19 level model had not produced a warming by the end of the integration on 22 March, but predicted a further cold spell in early March together with additional PSCs and ozone destruction. Since final warmings in the Arctic nearly always occur before this date, it 作者: Interregnum 時(shí)間: 2025-3-29 07:21
Concurrent Ozone and Temperature Trends Derived from Ozonesonde Stationsly significant surface warming over the past two decades. Above the South Pole, an observed strong cooling during November month can be simulated with a radiative transfer model under the concept of fixed dynamical heating, due to the observed ozone hole deepening one month earlier.作者: armistice 時(shí)間: 2025-3-29 11:27 作者: 增減字母法 時(shí)間: 2025-3-29 18:45
Ozone Chemistry Changes in the Troposphere and Consequent Radiative Forcing of Climate27 Tg/yr, caused mostly by anthropogenic emissions in the mid- latitude northern hemisphere and to a lesser extent by biomass burning emissions in the tropics. We calculate that the global O. burden in the troposphere has increased by a factor of 1.7, the CO burden by a factor of 2.5 and that of H.O作者: 頂點(diǎn) 時(shí)間: 2025-3-29 20:24
A GCM Study of the Climatic Effect of 1979–1992 Ozone Trende forcing expectations. Over the Arctic, a relatively small O. loss leads the model stratosphere to warm substantially during November-January. This is followed by a strong cooling in March-May. The result cannot be attributed exclusively to the radiative forcing. Rather it indicates the dominant ro作者: 潛伏期 時(shí)間: 2025-3-29 23:56 作者: 低能兒 時(shí)間: 2025-3-30 04:10
Unendliche Produkte holomorpher Funktionenions. However, the effect may be compensated for if cloudiness increases. A temperature increase of 4.2° C produced a global increase of 30% in lightning activity (70% over continental regions), which will increase both NO. and O. aloft. Finally, changes in convective activity may either increase or作者: 整頓 時(shí)間: 2025-3-30 12:11 作者: Gourmet 時(shí)間: 2025-3-30 13:59
Komplexe Zahlen und stetige Funktionenly significant surface warming over the past two decades. Above the South Pole, an observed strong cooling during November month can be simulated with a radiative transfer model under the concept of fixed dynamical heating, due to the observed ozone hole deepening one month earlier.作者: 暴發(fā)戶 時(shí)間: 2025-3-30 19:33
Konvergenzbegriffe der Funktionentheories has increased during the last decades. A primary contribution to this intensification due to the low latitude greenhaouse-gas effects with a positive feedback-loop via ozone chemistry and transport is suggested..Concluding, a comprehensive climate model including atmospheric chemistry in combinati作者: glowing 時(shí)間: 2025-3-31 00:11
https://doi.org/10.1007/3-7643-7430-627 Tg/yr, caused mostly by anthropogenic emissions in the mid- latitude northern hemisphere and to a lesser extent by biomass burning emissions in the tropics. We calculate that the global O. burden in the troposphere has increased by a factor of 1.7, the CO burden by a factor of 2.5 and that of H.O作者: 希望 時(shí)間: 2025-3-31 02:14
Potenzen und M?biustransformationene forcing expectations. Over the Arctic, a relatively small O. loss leads the model stratosphere to warm substantially during November-January. This is followed by a strong cooling in March-May. The result cannot be attributed exclusively to the radiative forcing. Rather it indicates the dominant ro作者: MIRTH 時(shí)間: 2025-3-31 08:06 作者: 打折 時(shí)間: 2025-3-31 12:45
1431-7125 ation of possible climatic effects over the last few decades resulting from anthropogenic ally-induced changes in atmospheric ozone. The initial quantitative estimates of their direct climatic effects indicate significant impacts, though large uncertainties exist and studies using general circulatio作者: 亞當(dāng)心理陰影 時(shí)間: 2025-3-31 16:10 作者: 大溝 時(shí)間: 2025-3-31 20:42 作者: arousal 時(shí)間: 2025-3-31 23:16
Climate Modelingusing general circulation models (GCMs). These models can be used for sensitivity studies of the climatic response to prescribed ozone changes, however they are not yet adequate for climate prediction purposes with respect to these problems.作者: myriad 時(shí)間: 2025-4-1 05:28 作者: 感染 時(shí)間: 2025-4-1 06:40
Bestimmte Integrale und Residuenkalküld September. This phenomenon is observed more frequently in recent years as compared to the 70’s. The contribution (in terms of percentage) of stratospheric intrusions associated with the polar front to the tropospheric ozone budget, as observed from the ozone soundings, shows an annual Variation with a maximum in June and July.
