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Emissions irrelevant to future climate change?

A new study published in Carbon Balance and Management found that the link between carbon cycle and human-induced emissions may only be relevant for several centuries. The research suggests that even weak but continuing emissions can lead to eventual saturation of climate-carbon cycle feedback, regardless of when emissions peak.

SourceBMC (BioMed Central)·JournalCarbon Balance and Management·DateApr 27, 2008

Studying rivers for clues to global carbon cycle

A Northwestern University professor is studying rivers to understand how organic carbon is processed and consumed by microorganisms, revealing that it's a bigger component of global carbon cycling than thought. The study provides a framework for assessing these processes and sheds light on the internal cycling of carbon in rivers.

SourceNorthwestern University·JournalNature Geoscience·DateFeb 8, 2008

Earth's soils bear unmistakable footprints of humans

A new global overview by Duke University soil scientist Daniel Richter emphasizes the need to address soil health due to increased cultivation, grazing, and logging. The study highlights the importance of long-term observation and analysis to understand how to sustain soils and minimize adverse effects on the environment.

SourceDuke University·JournalSoil Science·DateJan 25, 2008

Fossil wood gives vital clues to ancient climates

A recent study using high-resolution stable-isotope analysis from 95-million-year-old fossilized wood found that the mid-Cretaceous period was not a super-greenhouse, but rather had a short-lived glaciation. This new information may help us understand how the biosphere will respond to human-generated alterations of CO2 concentration.

SourceMcMaster University·JournalGeology·DateFeb 23, 2006

AGU journal highlights - 13 December 2005

Researchers studied hurricane-force wind estimation using synthetic aperture radar and found a newly-developed model outperforms previous methods. Additionally, weakened thermohaline circulation led to increased snow cover over Europe due to reduced atmospheric circulation and changed climate influences. The Arctic Ocean's change also ...

SourceAmerican Geophysical Union·JournalGeophysical Research Letters·DateDec 14, 2005

New evidence extends greenhouse gas record from ice cores by 50 percent, adding 210,000 years

The new ice core analysis provides insights into Antarctic climate and greenhouse gas concentrations during the most recent warm period, known as Marine Isotope Stage 11. This analog warm period occurred between 420,000 and 400,000 years ago and shares similarities with our current warm period due to similar Earth-Sun configurations.