• Nenhum resultado encontrado

Cloud-Aerosol-Radiation (CAR) ensemble modeling system

N/A
N/A
Protected

Academic year: 2016

Share "Cloud-Aerosol-Radiation (CAR) ensemble modeling system"

Copied!
69
0
0

Texto

Loading

Referências

Documentos relacionados

Simulated model fields, including liquid water path (LWP), ice water path, cloud fraction, shortwave and longwave cloud forcing, precipitation, water vapor, and cloud droplet

fire aerosol radiative effect (RE) at TOA, radiative effects due to aerosol–radiation interactions (REari), due to aerosol–cloud interactions (REaci), surface-albedo changes (REsac)

We perturb aerosol and meteorological properties within an observationally-constrained LES and determine the cloud response, focusing on changes in liquid water path (LWP), bulk

di ff erences due to cloud parameterization schemes, in CTL and MAC, the other is the influence of aerosol activation and associated cloud particle numbers and sizes; how- ever, the

A multiple linear regression is performed to identify the dependence of α in cloudy scenes on cloud liquid water path (LWP) and aerosol optical depth (AOD), using the

Overall size statistics of the background aerosol particles (left), cloud ice residues (middle) and cloud droplet residues (right) detected with the SPLAT instrument (upper row) and

The well- predicted aerosol quantities, such as aerosol number, mass composition and optical properties, and the inclusion of full aerosol-cloud couplings lead to

P ¨oschl, U.: Aerosol- and updraft-limited regimes of cloud droplet formation: influence of par- ticle number, size and hygroscopicity on the activation of cloud condensation