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Everything about The Claw Hypothesis totally explained

The CLAW hypothesis proposes a feedback loop that operates between ocean ecosystems and the Earth's climate. The hypothesis specifically proposes that particular phytoplankton that produce dimethyl sulfide are responsive to variations in climate forcing, and that these responses lead to a negative feedback loop that acts to stabilise the temperature of the Earth's atmosphere. The CLAW hypothesis was originally proposed by Robert Charlson, James Lovelock, Meinrat Andreae and Stephen Warren, and takes its acronym from the first letter of their surnames.

The CLAW hypothesis

[[Image:CLAW_hypothesis_graphic_1_AYool.png|thumb|200px|right|Schematic diagram of the CLAW hypothesis (Charlson et al., 1987).
   Some subsequent studies of the CLAW hypothesis have uncovered some evidence to support its mechanism, although this isn't unequivocal. Other researchers have suggested that a CLAW-like mechanism may operate in the Earth's sulfur cycle without the requirement of an active biological component.

The Anti-CLAW hypothesis

[[Image:CLAW_hypothesis_graphic_2_AYool.png|thumb|200px|right|Schematic diagram of the anti-CLAW hypothesis (Lovelock, 2006).
   Under future global warming, increasing temperature may stratify the world ocean, decreasing the supply of nutrients from the deep ocean to its productive euphotic zone. Consequently, phytoplankton activity will decline with a concommitant fall in the production of DMS. In a reverse of the CLAW hypothesis, this decline in DMS production will lead to a decrease in cloud condensation nuclei and a fall in cloud albedo. The consequence of this will be further climate warming which may lead to even less DMS production (and further climate warming ...). The figure to the right shows a summarising schematic diagram.
   Evidence for the anti-CLAW hypothesis is constrained by similar uncertainties as those of the sulfur cycle feedback loop of the CLAW hypothesis. However, researchers simulating future oceanic primary production have found evidence of declining production with increasing ocean stratification.
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