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Open AccessJournal ArticleDOI

Observed 20th century desert dust variability: impact on climate and biogeochemistry

TLDR
In this paper, the authors present observational estimates of desert dust based on pa- leodata proxies showing a doubling of the amount of dust during the 20th century over much, but not all the globe.
Abstract
Desert dust perturbs climate by directly and in- directly interacting with incoming solar and outgoing long wave radiation, thereby changing precipitation and tempera- ture, in addition to modifying ocean and land biogeochem- istry. While we know that desert dust is sensitive to pertur- bations in climate and human land use, previous studies have been unable to determine whether humans were increasing or decreasing desert dust in the global average. Here we present observational estimates of desert dust based on pa- leodata proxies showing a doubling of desert dust during the 20th century over much, but not all the globe. Large uncertainties remain in estimates of desert dust variability over 20th century due to limited data. Using these ob- servational estimates of desert dust change in combination with ocean, atmosphere and land models, we calculate the net radiative effect of these observed changes (top of at- mosphere) over the 20th century to be 0.14± 0.11 W/m 2 (1990-1999 vs. 1905-1914). The estimated radiative change

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Book ChapterDOI

Anthropogenic and Natural Radiative Forcing

TL;DR: Myhre et al. as discussed by the authors presented the contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change (IPCC) 2013: Anthropogenic and Natural Radiative forcing.
Book ChapterDOI

Carbon and Other Biogeochemical Cycles

TL;DR: For base year 2010, anthropogenic activities created ~210 (190 to 230) TgN of reactive nitrogen Nr from N2 as discussed by the authors, which is at least 2 times larger than the rate of natural terrestrial creation of ~58 Tg N (50 to 100 Tg nr yr−1) (Table 6.9, Section 1a).
Journal ArticleDOI

The physics of wind-blown sand and dust

TL;DR: The physics of aeolian saltation, the formation and development of sand dunes and ripples, the physics of dust aerosol emission, the weather phenomena that trigger dust storms, and the lifting of dust by dust devils and other small-scale vortices are reviewed.
Journal ArticleDOI

Global Scale Attribution of Anthropogenic and Natural Dust Sources and their Emission Rates Based on MODIS Deep Blue Aerosol Products

TL;DR: In this article, a global-scale high-resolution (0.1°) mapping of sources based on Moderate Resolution Imaging Spectroradiometer (MODIS) Deep Blue estimates of dust optical depth in conjunction with other data sets including land use is presented.
References
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Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica

TL;DR: The recent completion of drilling at Vostok station in East Antarctica has allowed the extension of the ice record of atmospheric composition and climate to the past four glacial-interglacial cycles.
Journal ArticleDOI

Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica

TL;DR: The recent completion of drilling at Vostok station in East Antarctica has allowed the extension of the ice record of atmospheric composition and climate to the past four glacial-interglacial cycles as discussed by the authors.
Journal ArticleDOI

Environmental characterization of global sources of atmospheric soil dust identified with the nimbus 7 total ozone mapping spectrometer (toms) absorbing aerosol product

TL;DR: In this article, the authors used the Total Ozone Mapping Spectrometer (TOMS) sensor on the Nimbus 7 satellite to map the global distribution of major atmospheric dust sources with the goal of identifying common environmental characteristics.
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