Constraints from 210Pb and 7Be on wet deposition and transport in a global three‐dimensional chemical tracer model driven by assimilated meteorological fields

By Hongyu Liu, D. J. Jacob, I. Bey, R. Yantosca. 2001

739 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/4af87d52748dbbb1ceb7c5cac23f17042806eebd

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. Ulrike Lohmann
2. C. Hoose
3. Xiaohong Liu
4. Martin Wild
5. Fangqun Yu
6. J. Penner
7. M. Andreae
8. Johannes Quaas

In Global and Planetary Change

1. Ulrike Lohmann
2. C. Hoose
3. Xiaohong Liu
4. Martin Wild
5. M. Andreae
6. Johannes Quaas
7. G. Luo
8. Fangqun Yu

Citations in the corpus

• Exploiting simultaneous observational constraints on mass and absorption to estimate the global direct radiative forcing of black carbon and brown carbon (2014, background): “…model dependent on the local surface type and meteorological conditions (Zhang, 2001) and wet removal mainly follows the scheme described by Liu et al. (2001), which includes both in-cloud rainout (only for hydrophilic BC) and below-cloud washout (for all BC) for both large scale and…”
• Effects of the physical state of tropospheric ammonium-sulfate-nitrate particles on global aerosol direct radiative forcing (2003, neutral): “Aerosol and gas losses by wet deposition include scavenging in convective updrafts/anvils and rainout/washout from large-scale precipitation (Liu et al., 2001).”
• Tropospheric Ozone Determined from Aura OMI and MLS: Evaluation of Measurements and Comparison with the Global Modeling Initiative's Chemical Transport Model (2006, methodology): “ing algorithm as described by Liu et al. [2001] and the dry deposition scheme as described by Wang et al. [1998], which follows the methodology of Wesely et al.”
• Contrasting the direct radiative effect and direct radiative forcing of aerosols (2014, background): “Wet deposition of soluble aerosols and gases includes contributions from scavenging in convective updrafts, rainout, and washout (Liu et al., 2001).”
• Why are there large differences between models in global budgets of tropospheric ozone (2007, methodology): “20 21 22 results reported in literature: Houweling et al. [1998] found that including NMVOCs hardly affected the tropospheric OH burden; Roelofs and Lelieveld [2000] reported that tropospheric OH decreases by about 8% when NMVOCs are accounted for; Poisson et al. [2000] and von Kuhlmann et al. [2004”
• Modelling the effect of size on the aerial dispersal of microorganisms (2012, neutral): “Wet deposition uses the scheme of Liu et al. (2001), which includes scavenging in convective updrafts, rainout and washout from large-scale precipitation and convective anvils.”
• Export efficiency of black carbon aerosol in continental outflow: Global implications (2005, methodology): “The scheme was originally tested by simulation of aerosol radionuclides [Liu et al., 2001] and also yields a good simulation of soluble species concentrations in the United States [Park et al., 2003, 2004] and in North American outflow [Li et al., 2004].”
• Reevaluation of Mineral aerosol radiative forcings suggests a better agreement with satellite and AERONET data (2006, background): “Based on Mari et al. (2000) and Liu et al. (2001), we adopt Cpr=5×10−3 m s−1, w=10 m s−1 leadingα=5×10−4 m−1.”
• Simulation of particle size distribution with a global aerosol model: contribution of nucleation to aerosol and CCN number concentrations (2009, methodology): “Wet deposition in GEOS-Chem, as described in Liu et al. (2001), includes scavenging in convective updrafts, rainout and washout from convective anvils and large-scale precipitation, and returning to the atmosphere following evaporation.”
• Sulfur, sea salt, and radionuclide aerosols in GISS ModelE (2006, methodology): “ Liu et al. [2001] found improved radionuclide simulation at the South Pole when they did not suppress scavenging by frozen precipitation.”
• Analysis and quantification of the diversities of aerosol life cycles within AeroCom (2005, neutral): “DLR Lohmann et al. (1999); Lohmann (2002); Lohmann and K̈archer (2002) Tiedtke (1989) modified after Brinkop and Sausen (1997) strat&conv: nucl: impact scav by Brownian motion, accm: activation (Henning et al.”
• Enhanced Solar Energy Absorption by Internally-Mixed Black Carbon in Snow Grains (2012, background): “…0◦C to −40◦C, and is constant at 0.1 below−40◦C. Stratiform precipitation collects cloud-borne and interstitial aerosols through in-cloud and below-cloud scavenging processes in both CAM5 (Barth et al., 2000; Rasch et al., 2000; Liu et al., 2012), and IMPACT (Mari et al., 2001; Liu et al., 2001).”
• Influences of in-cloud aerosol scavenging parameterizations on aerosol concentrations and wet deposition in ECHAM5-HAM (2009, methodology): “4.1 Simulation of 210Pb and 7Be25 7Be and 210Pb have been simulated in global models, and used as passive tracers for the validation of deposition parameterizations (e.g., Brost et al., 1991; Liu et al., 2001; Feichter et al., 1991; Koch et al., 1996, 2006).”
• Global observations of aerosol‐cloud‐precipitation‐climate interactions (2014, background): “The term “rainout” usually refers to in-cloud scavenging of aerosols by precipitation, whereas “washout” refers to below-cloud scavenging by precipitation [e.g., Liu et al., 2001; Seinfeld and Pandis, 1998].”
• Tropospheric chemistry in the integrated forecasting system of ECMWF (2014, methodology): “The module for wet deposition in C-IFS is based on the Harvard wet deposition scheme (Jacob et al., 2000; Liu et al., 2001).”