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Titlebook: Biogeochemistry of Global Change; Radiatively Active T Ronald S. Oremland (Chairman) Book 1993 Chapman & Hall, Inc. 1993 Atmospheric chemis

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發(fā)表于 2025-3-21 18:54:05 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
期刊全稱Biogeochemistry of Global Change
期刊簡(jiǎn)稱Radiatively Active T
影響因子2023Ronald S. Oremland (Chairman)
視頻videohttp://file.papertrans.cn/188/187045/187045.mp4
圖書(shū)封面Titlebook: Biogeochemistry of Global Change; Radiatively Active T Ronald S. Oremland (Chairman) Book 1993 Chapman & Hall, Inc. 1993 Atmospheric chemis
影響因子Certain trace gases in the atmosphere are able to absorbelectromagnetic energy from the reflection of solar radiation fromthe Earth‘s surface. These gases have been increasing steadily andthere is concern that they will change global climatic conditions bywarming the atmosphere--the so-called ``greenhouse effect.‘‘ Many ofthese gases originate from biological systems. The Biogeochemistry ofGlobal Change discusses the role of radiative trace gases in thisprocess. The disciplines covered in the book include microbiology,geochemistry, atmospheric chemistry, plant physiology, oceanographyand limnology, and soil science. This diversity allows forcross-fertilization, achieving a better understanding of the complexmechanisms for biological and chemical formation, the destruction oftrace gases, and the manipulation of ecosystems. Some of the topicscovered include: biological mechanisms of formation and destructionof various ``greenhouse‘‘ gases (such as methane, nitrous oxide,carbon dioxide, dimethylsulfide, and chlorofluorocarbons); theoutward and consumptive flux of trace gases from marine andterrestrial systems (including anthropogenic sources); global tracegas modeling studies; the atm
Pindex Book 1993
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Ice Core Records as a Key to Understanding the History of Atmospheric Trace Gasesthe last 150,000 years). Of special interest is the most direct evidence of past changes in radiatively active trace gases found in the ice record. We present here a review of the results concerning three of the main radiatively active gases: CO., CH., and N.O..The record indicates that the three ga
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A Time-Dependent Two-Dimensional-Model Study of the Trend in Atmospheric Methane. Possibilities include increased emissions from the use of fossil fuel, landfills, biomass burning, domestic cattle, and rice paddies. Another possibility is a reduction in the photochemical removal rate of CH. in the atmosphere due to decreasing concentrations of OH. Such reductions could result f
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Long-Term Effects of Fossil-Fuel-Burning and Deforestation on Levels of Atmospheric CO2numerical simulations of atmospheric CO. concentrations over the next few hundreds to hundreds of thousands of years for various patterns of fossil-fuel consumption and land use. The computer model predicts that atmospheric CO. concentrations could exceed 2000 ppm (parts per million) within the next
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Models of Oceanic and Terrestrial Sinks of Anthropogenic CO2: A Review of the Contemporary Carbon Cyes the CO. sinks to remove 2.9–5.0 GtC/yr, an amount equal to 43% of the fossil fuel plus 100% of the deforestation inputs. Oceanic uptake estimated directly from data on air-sea differences in the partial pressures of CO. is ~1.6 GtC/yr; uncertainties in this estimate due to inadequate sampling bot
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Agriculture, the Global Nitrogen Cycle, and Trace Gas Flux inadequate. Moreover, our knowledge of the budgets of other nitrogen-containing trace gases is worse than that for nitrous oxide. An analysis of the overall global nitrogen cycle and anthropogenic perturbations to it suggest that the global cycle has been altered to a greater extent than has nitrou
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