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[PDF] Top 20 The aerosol-climate model ECHAM5-HAM

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The aerosol-climate model ECHAM5-HAM

The aerosol-climate model ECHAM5-HAM

... Mcmurry, P., Noone, K., Dowd, C., Penner, J., Pszenny, A., Putaud, J., Quinn, P., Schurath, U., Seinfeld, J., Sievering, H., Snider, J., Sokolik, I., Stratmann, F., Dingenen, R. V., Westphal, D., Wexler, A., ... See full document

73

Aerosol nucleation and its role for clouds and Earth's radiative forcing in the aerosol-climate model ECHAM5-HAM

Aerosol nucleation and its role for clouds and Earth's radiative forcing in the aerosol-climate model ECHAM5-HAM

... Acknowledgements. We thank K. O’Brien (Northern Arizona University) for providing data of atmospheric ionization by galactic cosmic rays, N. A. Tsyganenko (Saint Petersburg State Uni- versity) for providing the ... See full document

48

<sup>10</sup>Be in late deglacial climate simulated by ECHAM5-HAM – Part 2: Isolating the solar signal from <sup>10</sup>Be deposition

<sup>10</sup>Be in late deglacial climate simulated by ECHAM5-HAM – Part 2: Isolating the solar signal from <sup>10</sup>Be deposition

... in climate data analysis to detect pat- terns such as the North Atlantic oscillation or the Southern Annular Mode in sea level pressure data, among various ...Because the global 10 Be ... See full document

31

Aerosol indirect effects in a multi-scale aerosol-climate model PNNL-MMF

Aerosol indirect effects in a multi-scale aerosol-climate model PNNL-MMF

... for the column-integrated aerosol number concentra- tions to calculate ACI in the MMF model for cloud droplet number concentrations, LWP, and cloud fraction, following the same approach ... See full document

61

Global impact of contemporary smoke aerosols from landscape fires on climate and the Hadley circulation

Global impact of contemporary smoke aerosols from landscape fires on climate and the Hadley circulation

... contribute the most to the large response in the Eastern Pacific, for example could be done by isolating emissions from Africa, South America and other high burn- ing regions in individual ... See full document

40

Aerosol-climate interactions in the Norwegian Earth System Model &amp;ndash; NorESM

Aerosol-climate interactions in the Norwegian Earth System Model &ndash; NorESM

... for the individual modelled species for the sensitivity tests defined in Table ...from the Ctrl and the Online experi- ments are from the simulation year ...7. The sensitivity ... See full document

87

Implementation of the chemistry module MECCA (v2.5) in the modal aerosol version of the Community Atmosphere Model component (v3.6.33) of the Community Earth System Model

Implementation of the chemistry module MECCA (v2.5) in the modal aerosol version of the Community Atmosphere Model component (v3.6.33) of the Community Earth System Model

... result, the need to more explicitly resolve many of the physical and chemi- cal processes that previously operated below the resolution and within the uncertainty ranges of these modeling sys- ... See full document

8

Implementation of the chemistry module MECCA (v2.5) in the modal aerosol version of the Community Atmosphere Model component (v3.6.33) of the Community Earth System Model

Implementation of the chemistry module MECCA (v2.5) in the modal aerosol version of the Community Atmosphere Model component (v3.6.33) of the Community Earth System Model

... of the work presented here, CCSM has been renamed the Com- munity Earth System Model, ...CESM). The coupled modeling system was designed to investigate the role of aqueous processes and ... See full document

19

Development of prognostic aerosol–cloud interactions combining a chemistry transport model and a regional climate model

Development of prognostic aerosol–cloud interactions combining a chemistry transport model and a regional climate model

... in: Climate Change 2013: The Physical Science ...to the Fifth Assessment Report of the Intergovern- mental Panel on Climate Change, edited by: Stocker, ... See full document

37

Desert dust and anthropogenic aerosol interactions in the Community Climate System Model coupled-carbon-climate model

Desert dust and anthropogenic aerosol interactions in the Community Climate System Model coupled-carbon-climate model

... Physical climate changes modify the ocean and land bio- geochemistry through changes in winds (oceans) and precip- itation (land and oceans), for ...addition, the ocean model allows incoming ... See full document

28

The multi-scale aerosol-climate model PNNL-MMF: model description and evaluation

The multi-scale aerosol-climate model PNNL-MMF: model description and evaluation

... In the ECPP approach, the CRM cells on each GCM grid column are first clas- sified into 12 different classes, according their vertical velocities, hydrometer mixing ratios, and precipitating rates ...Once ... See full document

71

&lt;sup&gt;10&lt;/sup&gt;Be in last deglacial climate simulated by ECHAM5-HAM &amp;ndash; Part 1: Climatological influences on &lt;sup&gt;10&lt;/sup&gt;Be deposition

<sup>10</sup>Be in last deglacial climate simulated by ECHAM5-HAM &ndash; Part 1: Climatological influences on <sup>10</sup>Be deposition

... because the model simulations present two 30 yr snapshots during this ...However, the model simulations presented here have been fully ... See full document

29

Global distribution and climate forcing of marine organic aerosol: 1. Model improvements and evaluation

Global distribution and climate forcing of marine organic aerosol: 1. Model improvements and evaluation

... over the marine environ- ment is predominantly associated with primary emissions from the sea surface, while WSOM is of secondary origin (Ceburnis et ...to the formation of WSOM (Rinaldi et ...our ... See full document

17

Global distribution and climate forcing of marine organic aerosol – Part 1: Model improvements and evaluation

Global distribution and climate forcing of marine organic aerosol – Part 1: Model improvements and evaluation

... to the CCN budget can be important throughout the whole ...(1) the organic mass fraction of sea spray approaches 100 % (pure organics) for particles below 100 nm in dry diameter, reflecting ... See full document

47

Global distribution and radiative forcing of soil dust aerosols in the Last Glacial Maximum simulated by the aerosol climate model

Global distribution and radiative forcing of soil dust aerosols in the Last Glacial Maximum simulated by the aerosol climate model

... of the soil moisture, but they were still lower than values reported from ice ...for the dust emission (e.g., vegetation) could also improve the LGM dust ...that the simulated dust deposition ... See full document

38

Climate model bias correction and the role of timescales

Climate model bias correction and the role of timescales

... for the daily nor the monthly mean standard deviation and there is no clear dominance of a positive or negative ...However, the ECHAM5 model appears to generally underestimate ... See full document

36

Observed and simulated estimates of the meridional overturning circulation at 26.5&amp;deg; N in the Atlantic

Observed and simulated estimates of the meridional overturning circulation at 26.5&deg; N in the Atlantic

... by the NOAA Office of Climate Observations. The wind-stress data were obtained from Centre ERS d’Arquivage et de Traitment the Institut Franc¸ais de Recherche pour l’Exploration de la Mer in ... See full document

35

Stable water isotopes in the coupled atmosphere–land surface model ECHAM5-JSBACH

Stable water isotopes in the coupled atmosphere–land surface model ECHAM5-JSBACH

... in the hydrological cycle of the coupled atmosphere–land surface model ...ECHAM5-JSBACH. The ECHAM5-JSBACH-wiso model was run under present-day climate conditions ... See full document

18

Black carbon reduction will weaken the aerosol net cooling effect

Black carbon reduction will weaken the aerosol net cooling effect

... estimate the influence of removing some sources of BC and other co-emitted species on the aerosol radiative effect by using an aerosol-climate coupled model ...with the ... See full document

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Aerosol size-dependent below-cloud scavenging by rain and snow in the ECHAM5-HAM

Aerosol size-dependent below-cloud scavenging by rain and snow in the ECHAM5-HAM

... tion model (GCM) developed at the Max-Planck Institute for Meteorology (Roeckner et ...from the model of the European Centre for Medium Range Weather Forecasting ...(ECMWF). The ... See full document

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