Dimethylsulfide Affecting Climate


 


Climatic Effects on Oceanic DMS Producers

Wong, C.-S., Wong, S.-K. E., Pena, A. and Levasseur, M. 2006. Climatic effect on DMS producers in the NE sub-Arctic Pacific: ENSO on the upper ocean. Tellus 58B: 319-326.

Dimethylsulfide (DMS), which is derived from its algal precursor dimethylsulphoniopropionate (DSMP), is a climatically-important trace gas that has its origin in the activity of certain types of marine phytoplankton and is believed to play a major role in keeping earth's temperature within bounds that are conducive to the continual existence of life. Very briefly, and rather simplistically, in response to an initial warming (caused by an increase in the air's CO2, the climate-stabilizing mechanism begins with a warming-induced increase in the productivity of certain marine phytoplankton, which leads to a greater production of oceanic DMS and its release to the atmosphere, which boosts the number of gas-to-particle conversions, increasing the atmosphere's population of cloud condensation nuclei and, ultimately, the albedos of marine stratus and altostratus clouds via a narrowing of the cloud droplet spectrum and a decrease in the mean radius of the cloud droplets, both of which phenomena tend to counteract the initial impetus for warming.

From 1996 to 2001 the authors recorded DMS concentrations and physical oceanographic data at ocean stations P26 (50°N, 145°W) and P20 (49°34'N, 138°40'W) in the Northeast Pacific Ocean, after which they analyzed the data in a number of different ways. What was learned Wong's work confirmed that as the sea surface temperature of a region rises, "the stratification of the upper water column intensifies and oceanic upwelling weakens," such that "in the nutrient-rich waters of the sub-Arctic Pacific, higher stratification and shallower mixed layer favor the growth of small-sized phytoplankton such as flagellates, dinoflagellates and coccolithophorids." And noting that "most prolific DMSP producers are members of these phytoplankton groups," they say that, "consequently, the local ecosystem is shifted towards one with structure and function adapted to [increasing] production of DMSP and DMS."
 



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