Big Chemical Encyclopedia

Chemical substances, components, reactions, process design ...

Articles Figures Tables About

Change climatic effects

Winder M, Schindler DE (2004) Climatic effects on the phenology of lake processes. Global Change Biol 10 1844-1856... [Pg.93]

Hayhoe, K. Kheshgi, H.S. Jain, A.K. Wuebbles, D.J. Substitution of natural gas for coal Climatic effects of utility sector emissions. Clim. Change. 2002, 54,107-139. [Pg.302]

Harvey, L.D.D., Declining temporal effectiveness of carbon sequestration, implications for compliance with the United National framework convention on climate change, Climate Change, 63(3), 259,2004. [Pg.599]

Base cations are mobilized by weathering and cation exchange reactions that neutralize acids in the watershed. They respond therefore indirectly to changes in sulphate and nitrate concentrations. In fact, if acid anion concentrations (mainly sulphate) decrease, base cations are also expected to decrease. However, in the last few years an increase of the occurrence of alkaline rain episodes (probably due to climatic effects) has been observed and it is likely that calcareous Saharan dust, rich in base cations, is responsible for it [27]. Accelerated weathering, resulting from recent climate warming may also contribute to higher base cation concentrations [28]. [Pg.133]

Global climate change (greenhouse effect) is considered one of the most urgent environmental... [Pg.274]

A great variety of possible chemical and climatic effects of aircraft have been investigated in recent years. In this study, aircraft-induced changes in NOy, H20 and ozone have been calculated. The study has contributed to the IPCC report on the atmospheric effects of aviation, which gives a comprehensive introduction into the aircraft issue [3]. [Pg.91]

Much of what is currently known about the Earth s climate comes from the application of stable isotopes collected from ocean drill cores in marine sediments (e.g., Zachos et al. 2001). These isotopic data sets provide detailed records of how the Earth s oceans have responded to changing climate and are extremely valuable in assessing global climate histories down to millennial scales. Similar detailed isotopic records for terrestrial systems are, however, uncommon and frequently continuous terrestrial climate records that span millions to tens of millions of years are not preserved in the terrestrial geologic record. With the advent of paleoaltimetry studies targeted directly at the coupled isotopic effects of changes in climate... [Pg.90]

In addition to long-term and large-scale climatic effects, the annual variation in weather conditions also affected the amount and turnover of plant residues and thus the chemical composition SOM sampled at a certain date (Leinweber et al., 1994, 1995). Figure 14.19 shows the ion intensities for carbohydrates in two plots of the Eternal Rye Cultivation experiment at Halle, Saxony-Anhalt, Germany. In 1958, parts of the former rye monoculture were shifted into maize monoculture. This resulted in decreases in the ion intensities for carbohydrates. In the plot that remained under rye monoculture the ion intensities for carbohydrates increased initially. For several time periods, the changes in ion intensities were roughly parallel for the two plots, which is considered as evidence for annual variations in the decomposition dynamics. For some time (1993 to 1997), there was no significant difference between the rye and maize plots in the ion intensities for carbohydrates, but the... [Pg.576]

Global Warming An increase in the near-surface temperature of the Earth. Global warming has occurred in the distant past as the result of natural influences, but the term is most often used to refer to a theory that warming occurs as a result of increased use of hydrocarbon fuels by man. See Climate Change (Greenhouse Effect). ... [Pg.19]

Woodwell G.M. (1983) Biotic effects on atmospheric carbon dioxde A review and projection in changing climate. National Academy of Sciences Press, Washington, D.C., 216-241. [Pg.678]

The ratio of certain stable isotopes, principally 13C/12C and 180/160, varies with geographical location where climatic effects change the proportions of the isotopes available to plants. Stable isotope measurements can be carried out... [Pg.85]


See other pages where Change climatic effects is mentioned: [Pg.15]    [Pg.24]    [Pg.31]    [Pg.245]    [Pg.392]    [Pg.460]    [Pg.73]    [Pg.78]    [Pg.56]    [Pg.24]    [Pg.33]    [Pg.40]    [Pg.54]    [Pg.296]    [Pg.297]    [Pg.323]    [Pg.44]    [Pg.193]    [Pg.21]    [Pg.53]    [Pg.100]    [Pg.93]    [Pg.15]    [Pg.24]    [Pg.31]    [Pg.369]    [Pg.108]    [Pg.16]    [Pg.67]    [Pg.103]    [Pg.146]    [Pg.19]    [Pg.423]    [Pg.15]    [Pg.471]    [Pg.266]    [Pg.15]   
See also in sourсe #XX -- [ Pg.240 , Pg.246 , Pg.247 ]




SEARCH



Climate Change aerosol particles, direct effects

Climate Change aerosol particles, indirect effects

Climate change

Climate change doubling effects

Climate change greenhouse effect

Climate change temperature effects

Climate, effect

Climatic change

Climatic effects

Global Climate Change Greenhouse Effect

Global Climate Change The Greenhouse Effect

Greenhouse effect climate change and

Reservoirs, climate change effects

Terrestrial vegetation climatic change, effect

© 2024 chempedia.info