Material in this section originates from the following categories in our Subject Index:
Aerosols (Biological: Aquatic, DMS)
Dimethyl Sulfide
Feedback Factors (Dimethylsulfide)
Oceans (Dimethyl Sulfide)
Material preceded by an asterisk (*) was posted after this subject summary was written and therefore is not included in the summary. This material will be integrated into the summary at a later date.
* -- On the Climatic Benefits of Antarctic Polynyas
* -- Effects of Declining Arctic Sea Ice on Biogenic Sulfate Aerosols
Modeled Warming-Induced Changes in Oceanic DMS Production
Improving the Quantification of Oceanic DMS and DMSP
Oceanic Dimethylsulfide Production in a CO2-Enriched and Warmer World
Dimethylsulfide, Global Warming and the Arctic Ocean
Another Test of the CLAW Hypothesis
Marine Ecosystem Response to "Ocean Acidification" Due to Atmospheric CO2 Enrichment
Dimethylsulfide Production in the North Pacific Ocean
Elevated Atmospheric CO2 Concentrations Enhance Marine Production of DMS and CH2CII
Marine Phytoplankton and Clouds
Climatic Effects on Oceanic DMS Producers
Atmospheric DMS in Relation to Local Coral Cover
DMS and DMSP Associated with Great Barrier Reef Corals
The Capacity of Man and Nature to Control Climate Change
The World's Oceans Possess Not One CLAW, But Two
Demise of "The CLAW" Greatly Exaggerated
More Evidence that Algae Help to Regulate Earth's Climate
Aquatic Algae Are An Important Part of Earth's "Bio-Thermostat"
Dimethyl Sulfide: It's Role in Stabilizing Earth's Climate
Signs of One of the "Living Thermostats" that Moderate Climate Change
Adding to Our Knowledge of the Global-Ocean Biophysical Thermostat