Titlebook: Sediment Records of Biomass Burning and Global Change; James S. Clark,Hélène Cachier,Brian Stocks Conference proceedings 1997 Springer-Ver

尖酸好

書目名稱Sediment Records of Biomass Burning and Global Change影響因子(影響力)




書目名稱Sediment Records of Biomass Burning and Global Change影響因子(影響力)學科排名




書目名稱Sediment Records of Biomass Burning and Global Change網(wǎng)絡公開度




書目名稱Sediment Records of Biomass Burning and Global Change網(wǎng)絡公開度學科排名




書目名稱Sediment Records of Biomass Burning and Global Change被引頻次




書目名稱Sediment Records of Biomass Burning and Global Change被引頻次學科排名




書目名稱Sediment Records of Biomass Burning and Global Change年度引用




書目名稱Sediment Records of Biomass Burning and Global Change年度引用學科排名




書目名稱Sediment Records of Biomass Burning and Global Change讀者反饋




書目名稱Sediment Records of Biomass Burning and Global Change讀者反饋學科排名

格子架

An Introduction to Sediment Records of Biomass Burningcts atmospheric chemistry, the carbon cycle, and climate and may have done so for millions of years. Literature values place carbon sequestration during biomass burning in excess of 20% of the total anthropogenic C releases to the atmosphere, which, failing oxidative losses, would tie up the globe’s

insecticide

cardiovascular

拱形面包

Reconstruction Of Paleo-Fire Through Climate And Eco-System Modelsmass structure and function, and as a result, the carbon available for release in the atmosphere. The second part defines the relationship between ecosystem structure, weather, and fire behavior - the emission of carbon particulates. Modeling paleo - emissions of carbon from fire requires an underst

foliage

The Culture of Fire: An Introduction to Anthropogenic Fire Historyecological niche. Even today fire appears at the core of many popular scenarios for environmental apocalypse. Yet the larger history of fire—the varied ways human societies have sought to use and control fire, the trajectory of change over centuries if no millennia—is not well known..A useful scheme

迫擊炮

雀斑

N斯巴達人

Spongy-Bone

Biomass Burning Emissions and the Atmosphereon fires. Crutzen and Andreae (1990) have estimated that global emissions of pyrogenic smoke particles (50–150 Tg yr.) may currently exceed global sulfate aerosol produced from fossil fuel burning. These pyrogenic particulates are largely composed of carbonaceous materials (Crutzen and Andreae 1990,