@Article{HernandezPardoMMCAPPRVVWP:2021:ObSiVa,
author = "Hernandez Pardo, Lianet and Machado, Luiz Augusto Toledo and
Morrison, Hugh and Cecchini, Micael Amore and Andreae, Meinrat O.
and Poehlker, Christopher and Poeschl, Ulrich and Rosenfeld,
Daniel and Vendrasco, Eder Paulo and Voigt, Christiane and
Wendisch, Manfred and Poehlker, Mira L.",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {National Center for
Atmospheric Research} and {Universidade de S{\~a}o Paulo (USP)}
and {Max Planck Institute for Chemistry} and {Max Planck Institute
for Chemistry} and {Max Planck Institute for Chemistry} and {The
Hebrew University of Jerusalem} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {Deutsches Zentrum f{\"u}r Luft
und Raumfahr} and {Max Planck Institute for Chemistry} and {Max
Planck Institute for Chemistry}",
title = "Observed and Simulated Variability of Droplet Spectral Dispersion
in Convective Clouds Over the Amazon",
journal = "Journal of Geophysical Research: Atmospheres",
year = "2021",
volume = "126",
number = "20",
pages = "e2021JD035076",
month = "Oct.",
abstract = "In this study, the variability of the spectral dispersion of
droplet size distributions (DSDs) in convective clouds is
investigated. Analyses are based on aircraft measurements of
growing cumuli near the Amazon basin, and on numerical simulations
of an idealized ice-free cumulus. In cleaner clouds, the relative
dispersion epsilon, defined as the ratio of the standard deviation
to the mean value of the droplet diameter, is negatively
correlated with the ratio of the cloud water content (q(c)) to the
adiabatic liquid water content (q(a)), while no strong correlation
between epsilon and q(c)/q(a) is seen in polluted clouds. Bin
microphysics numerical simulations suggest that these contrasting
behaviors are associated with the effect of collision-coalescence
in cleaner clouds, and secondary droplet activation in polluted
clouds, in addition to the turbulent mixing of parcels that
experienced different paths within the cloud.
Collision-coalescence simultaneously broadens the DSDs and
decreases q(c), explaining the inverse relationship between
epsilon and q(c)/q(a) in cleaner clouds. Secondary droplet
activation broadens the DSDs but has little direct impact on q(c).
The combination of a rather modest DSD broadening due to weak
collision-coalescence with enhanced droplet activation in both
diluted and highly undiluted cloud regions may contribute to
maintain a relatively uniform epsilon within polluted clouds.
These findings can be useful for parameterizing the shape
parameter (mu) of gamma DSDs in bulk microphysics cloud-resolving
models. It is shown that emulating the observed mu-q(c)/q(a)
relationship improves the estimation of the collision-coalescence
rate in bulk microphysics simulations compared to the bin
simulations.",
doi = "10.1029/2021JD035076",
url = "http://dx.doi.org/10.1029/2021JD035076",
issn = "2169-8996 and 2169-897X",
language = "en",
targetfile = "Observed and Simulated Variability of Droplet Spectral Dispersion
in Convective Clouds Over the Amazon.pdf",
urlaccessdate = "12 maio 2024"
}