2001
DOI: 10.2307/4012776
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Dust, the thermostat: How tiny airborne particles manipulate global climate

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Cited by 35 publications
(15 citation statements)
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“…The current estimate for the quantity of arid soil that moves some distance in Earth's atmosphere each year is 2 billion metric tons (Perkins, 2001). Fifty to 75% of this quantity is believed to originate from the Sahara and Sahel (Moulin et al, 1997;Perry et al, 1997;Goudie and Middleton, 2001;Prospero and Lamb, 2003).…”
Section: Introductionmentioning
confidence: 99%
“…The current estimate for the quantity of arid soil that moves some distance in Earth's atmosphere each year is 2 billion metric tons (Perkins, 2001). Fifty to 75% of this quantity is believed to originate from the Sahara and Sahel (Moulin et al, 1997;Perry et al, 1997;Goudie and Middleton, 2001;Prospero and Lamb, 2003).…”
Section: Introductionmentioning
confidence: 99%
“…Owing to their various origins, dusts differ in color, size, shape, and chemical composition, and these differences strongly influence their behaviors (Perkins, 2001). Furthermore, whether derived from its point of origin or picked up along its pathway, dust may contain metals (iron, Jickells et al, 2005;Mahowald et al, 2005a;arsenic, Holmes and Miller, 2004;Ridgwell et al, 2005), radioisotopes (e.g., plutonium, Hirose et al, 2003;cesium-137, Papastefanou et al, 2001), bacteria (e.g., halophilic bacteria, Echigo et al, 2005), toxic chemicals (e.g., pesticides, herbicides), or viruses, which may harm wildlife, plants, and human beings.…”
Section: Introductionmentioning
confidence: 99%
“…Many studies have investigated the development of dust aerosols, and their transport and deposition, but researchers are just beginning to map out how the type and amount of dust in the atmosphere vary according to latitude, longitude, altitude, and time of year (Perkins, 2001). Dust aerosols still introduce large uncertainties into global climate change model results (Washington et al, 2003); for example, total mass burden estimates can differ by a factor of 4 (8-36 Tg) and emission estimates by a factor of 2 (1000-2150 Tg y −1 ) (Zender et al, 2004).…”
Section: Introductionmentioning
confidence: 99%
“…Desert storm activity is the most significant source of nonoccupational dust exposure in arid and semiarid regions of the world. It is estimated that 0.5 to 5 billion tons of desert topsoil is made airborne every year during high-wind desert storm events globally (50). Exposure to desert dust has been linked to many conditions, including silicosis and asthma (9,45,48,54).…”
mentioning
confidence: 99%