For the current climate, we calculate the reduction in wet
deposition by dust radiative forcing and find that the aerosol burden is increased only modestly.
Not exact matches
Glaser et al. show that
dust deposition mediated
by frequent tropical storms was an important source of nutrients for the Everglades until about 2800 years ago, when a climatic shift in the tropical Atlantic and Gulf of Mexico led to weather patterns that sharply decreased the level of
dust inputs and led to a drier climate and a gradual loss of soil phosphorus, carbon, and nitrogen.
Possible mechanisms include (iv) fertilization of phytoplankton growth in the Southern Ocean
by increased
deposition of iron - containing
dust from the atmosphere after being carried
by winds from colder, drier continental areas, and a subsequent redistribution of limiting nutrients; (v) an increase in the whole ocean nutrient content (e.g., through input of material exposed on shelves or nitrogen fixation); and (vi) an increase in the ratio between carbon and other nutrients assimilated in organic material, resulting in a higher carbon export per unit of limiting nutrient exported.
«Recently, the
deposition rates have been boosted
by the resuspension of radionuclides in deposited particles, the 239,240 Pu content of which may originate from
dusts from the East Asian continent deserts and arid areas.
The onsets of both abrupt Greenland warmings are slightly preceded
by decreasing Greenland
dust deposition, reflecting wetting of Asian deserts.
They showed the evidence to 77 domain experts (i.e., atmospheric chemists with expertise in condensation trails, and geochemists working on atmospheric
deposition of
dust and pollution), and asked about each of the claims made
by «SLAP theorists.»
Here we took a different approach
by seeking and applying
dust deposition observations from hotspots for
dust radiative and iron fertilization forcing: NH subtropical latitudes and the Southern Ocean.
Deposition of mineral
dust plays an important role in the biogeochemical cycle of the oceans,
by providing the nutrient iron, which affects ocean biogeochemistry with feedbacks to climate and
dust production (Jickells et al., 2005; Section 7.3.4.4).
The input of trace elements
by dust deposition is also of importance to terrestrial ecosystems.
2) That Planktos will be mitigating that shortfall
by replenishing marine iron micronutrients in concentrations similar to
dust storm
deposition is also a fact.