Electrification of precipitating systems over the Amazon: Physical processes of thunderstorm development


Autoria(s): ALBRECHT, Rachel I.; MORALES, Carlos A.; DIAS, Maria A. F. Silva
Contribuinte(s)

UNIVERSIDADE DE SÃO PAULO

Data(s)

19/10/2012

19/10/2012

2011

Resumo

This study investigated the physical processes involved in the development of thunderstorms over southwestern Amazon by hypothesizing causalities for the observed cloud-to-ground lightning variability and the local environmental characteristics. Southwestern Amazon experiences every year a large variety of environmental factors, such as the gradual increase in atmospheric moisture, extremely high pollution due to biomass burning, and intense deforestation, which directly affects cloud development by differential surface energy partition. In the end of the dry period it was observed higher percentages of positive cloud-to-ground (+CG) lightning due to a relative increase in +CG dominated thunderstorms (positive thunderstorms). Positive (negative) thunderstorms initiated preferentially over deforested (forest) areas with higher (lower) cloud base heights, shallower (deeper) warm cloud depths, and higher (lower) convective potential available energy. These features characterized the positive (negative) thunderstorms as deeper (relatively shallower) clouds, stronger (relatively weaker) updrafts with enhanced (decreased) mixed and cold vertically integrated liquid. No significant difference between thunderstorms (negative and positive) and nonthunderstorms were observed in terms of atmospheric pollution, once the atmosphere was overwhelmed by pollution leading to an updraft-limited regime. However, in the wet season both negative and positive thunderstorms occurred during periods of relatively higher aerosol concentration and differentiated size distributions, suggesting an aerosol-limited regime where cloud electrification could be dependent on the aerosol concentration to suppress the warm and enhance the ice phase. The suggested causalities are consistent with the invoked hypotheses, but they are not observed facts; they are just hypotheses based on plausible physical mechanisms.

Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)[04/09049-3]

Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)

PROEX-CAPES

European Commission[EVK2-CT-2001-00110 SMOCC]

Identificador

JOURNAL OF GEOPHYSICAL RESEARCH, v.116, 2011

0148-0227

http://producao.usp.br/handle/BDPI/27010

10.1029/2010JD014756

http://dx.doi.org/10.1029/2010JD014756

Idioma(s)

eng

Publicador

AMER GEOPHYSICAL UNION

Relação

Journal of Geophysical Research

Direitos

restrictedAccess

Copyright AMER GEOPHYSICAL UNION

Palavras-Chave #CONVECTIVE CLOUDS #TRMM-LBA #RADAR OBSERVATIONS #CHARGE-TRANSFER #CLIMATE-CHANGE #SOUTH-AMERICA #TOGA COARE #DEFORESTATION #AEROSOL #FOREST #Meteorology & Atmospheric Sciences
Tipo

article

original article

publishedVersion