@InProceedings{GuptaWanGiaBisJen:2022:EvDeCo,
author = "Gupta, Siddhant and Wang, Di{\'e} and Giangrande, Scott E. and
Biscaro, Thiago Souza and Jensen, Michael P.",
affiliation = "{Brookhaven National Laboratory} and {Brookhaven National
Laboratory} and {Brookhaven National Laboratory} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Brookhaven National
Laboratory}",
title = "The Evolution of Deep Convective Cloud Kinematic Properties over
the Amazon Rainforest with Cloud Lifetime",
year = "2022",
organization = "AGU Fall Meeting",
publisher = "AGU",
abstract = "Deep convective clouds (DCCs) redistribute energy and moisture in
Earths atmosphere and routinely constitute hazardous weather
events. The occurrence and intensity of DCCs largely depend on
environmental and aerosol conditions but the aerosol controls
remain uncertain due to inconclusive results from modeling studies
which suggest aerosols can either invigorate or enervate deep
convection. In this study, the uncertainty in aerosol impacts on
DCCs is addressed using observations of key convective properties
such as updraft strength at different DCC life cycle stages. The
Amazon basin features biogenic and anthropogenic aerosols with
frequent convective activity. Radiative effects and precipitation
associated with DCCs over the Amazon basin affect global
circulation and water cycle. The Atmospheric Radiation Measurement
(ARM) Mobile Facility was deployed 70 km from Manaus, Brazil,
during the Green Ocean Amazon (GoAmazon 2014/5, MAO) experiment,
an area covered by the Sistema de Prote{\c{c}}{\~a}o da
Amaz{\^o}nia Manaus S-band radar. Unique vertical velocity (w)
estimates from the ARM Radar Wind Profiler (RWP) at the MAO site
were used to gain insights into DCC kinematic properties. DCC life
cycle stages were identified by tracking convective cells in a
Lagrangian framework using the 2 km S-band radar reflectivity (Z)
and the Tracking and Object-Based Analysis of Clouds algorithm
(tobac). Precipitation associated with isolated DCCs was observed
on 76 days and 745 cells initiated and/or passed within 20 km of
the MAO site during their lifetime. The average Z and cell area
(A) increased from 41.6 dBZ and 44.3 km2 during the cell
developing stage to 44.2 dBZ and 106 km2 during the mature stage
and decreased to 38.9 dBZ and 81.4 km2 during cell dissipation.
Based on Z and w profiles from the RWP, the developing stage had
the highest Z and the strongest updrafts at lower- and mid-levels
followed by the mature stage. The mature stage had the strongest
updrafts at higher levels and downdrafts compensating for the
upward motion. The dissipation stage had the weakest updrafts and
downdrafts over the profile. On average, cell propagation speed
(u) increased from 6.3 to 7.3 m s-1 over cell lifetime. The dry
season had more intense, faster moving, and larger DCCs compared
to the wet season with up to 10%, 20%, and 37% higher Z, u, and A,
respectively.",
conference-location = "Chicago, IL",
conference-year = "12-16 Dec. 2022",
urlaccessdate = "28 abr. 2024"
}