Titlebook: Global Environmental Change; Bill Freedman Reference work 2014 Springer Science+Business Media Dordrecht 2014 Environmental Pollution.Glob

GRUEL

Changes in Atmospheric Carbon Dioxided to 387?ppm by the end of 2009, which is 38?% above the preindustrial levels. And, it keeps increasing at an accelerated rate. A large amount of anthropogenic CO. emitted into the air changes the balance between CO. sources and sinks. Fossil fuel combustion emission occupied 85?% of the anthropogen

disparage

Sea-Surface Temperatureal patterns of interannual ocean-climate interactions such as the El Ni?o/Southern Oscillation (ENSO) show the influence of SST variations on climate. Over longer periods the global SST has been warming since at least the nineteenth century, coincident with warming over land and changes in the Earth

輕快帶來(lái)危險(xiǎn)

Variations of Oceanic Heat Contentpatterns can be dominated by natural variations on decadal timescales, globally integrated ocean heat content responds primarily to external forcings such as anthropogenic global warming and major volcanic eruptions. The spatial patterns of future ocean heat content change and sea level rise (associ

hypertension

Ocean Currents and Circulation and Climate Changethat of the freshwater flux. Relatively small changes in atmospheric conditions can therefore lead to a spectacular reduction (collapse) of the strength of the Atlantic MOC. As the timescale of a collapse is only a few decades, the associated changes in heat transport may have a large impact on Euro

Aerophagia

Sea IceOn shorter time scales, additional perturbations are imposed by some other natural forcings and by changes in the heat transfer between sea ice, ocean, and atmosphere. Moreover, the recent decrease of the Arctic sea ice extent is partially due to human activities – the anthropogenic radiative forcin

不易燃

Ocean Acidification and Oceanic Carbon CyclingCO.” invades the oceans causing a decrease of seawater pH; this process is called “ocean acidification.” The lowered pH, but also the concomitant changes in other properties of the carbonate system, affects marine life and the cycling of carbon in the ocean.

malign

Carcinoma

unstable-angina

Lindsay Grey Cowell,Barry Smithhe intensity and frequency of natural SST variations, which will alter climate variations associated with those SST variations. Understanding how global warming may influence interannual SST variations is critical for improving climate prediction.

Anticlimax