A scaling theory for the size distribution of emitted dust aerosols suggests climate models underestimate the size of the global dust cycle.
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In Situ Liquid Cell Observations of Asbestos Fiber Diffusion in Water.Recently deglaciated high-altitude soils of the Himalaya: diverse environments, heterogenous bacterial communities and long-range dust inputs from the upper troposphere.Universality of fragment shapes.Characterizing the size and shape of sea ice floesSimulating the meteorology and PM10 concentrations in Arizona dust storms with the Weather Research and Forecasting model with Chemistry (Wrf-Chem).Global and regional importance of the direct dust-climate feedback.Anthropogenic combustion iron as a complex climate forcer.Fragmentation as an aggregation process: the role of defects.Universal characteristics of particle shape evolution by bed-load chipping.Quantifying particle size and turbulent scale dependence of dust flux in the Sahara using aircraft measurementsLagrangian dust model simulations for a case of moist convective dust emission and transport in the western Sahara region during Fennec/LADUNEXDevelopment and evaluation of a physics-based windblown dust emission scheme implemented in the CMAQ modeling systemA global comparison of GEOS-Chem-predicted and remotely-sensed mineral dust aerosol optical depth and extinction profilesSize-resolved adjoint inversion of Asian dustParticle Lifting Processes in Dust DevilsImpact of dust deposition on the albedo of Vatnajökull ice cap, IcelandSensitivity of the interannual variability of mineral aerosol simulations to meteorological forcing datasetSensitivity of the WRF-Chem (V3.6.1) model to different dust emission parametrisation: assessment in the broader Mediterranean regionMultiple sources of soluble atmospheric iron to Antarctic watersSubregional inversion of North African dust sourcesFacile Method for Determining the Aspect Ratios of Mineral Dust Aerosol by Electron MicroscopyModeling the effects of dust-radiative forcing on the movement of HurricaneHelene(2006)Development of a global aerosol model using a two-dimensional sectional method: 2. Evaluation and sensitivity simulationsEstimating the sensitivity of regional dust sources to sea surface temperature patternsSubstantial contribution of northern high-latitude sources to mineral dust in the ArcticDust plume formation in the free troposphere and aerosol size distribution during the Saharan Mineral Dust Experiment in North AfricaAerosol Deposition Impacts on Land and Ocean Carbon CyclesIs atmospheric phosphorus pollution altering global alpine Lake stoichiometry?Mineral dust aerosols over the Sahara: Meteorological controls on emission and transport and implications for modelingThe Influence of Topography on East African October to December Climate: Sensitivity Experiments with RegCM4Impact of vegetation and soil moisture seasonal dynamics on dust emissions over the Sahel
P2860
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P2860
A scaling theory for the size distribution of emitted dust aerosols suggests climate models underestimate the size of the global dust cycle.
description
2010 nî lūn-bûn
@nan
2010 թուականի Դեկտեմբերին հրատարակուած գիտական յօդուած
@hyw
2010 թվականի դեկտեմբերին հրատարակված գիտական հոդված
@hy
2010年の論文
@ja
2010年論文
@yue
2010年論文
@zh-hant
2010年論文
@zh-hk
2010年論文
@zh-mo
2010年論文
@zh-tw
2010年论文
@wuu
name
A scaling theory for the size ...... size of the global dust cycle.
@ast
A scaling theory for the size ...... size of the global dust cycle.
@en
type
label
A scaling theory for the size ...... size of the global dust cycle.
@ast
A scaling theory for the size ...... size of the global dust cycle.
@en
prefLabel
A scaling theory for the size ...... size of the global dust cycle.
@ast
A scaling theory for the size ...... size of the global dust cycle.
@en
P2860
P356
P1476
A scaling theory for the size ...... size of the global dust cycle.
@en
P2860
P304
P356
10.1073/PNAS.1014798108
P407
P50
P577
2010-12-28T00:00:00Z