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Luiz A. T. Machado
,
Maria A. F. Silva Dias
,
Carlos Morales
,
Gilberto Fisch
,
Daniel Vila
,
Rachel Albrecht
,
Steven J. Goodman
,
Alan J. P. Calheiros
,
Thiago Biscaro
,
Christian Kummerow
,
Julia Cohen
,
David Fitzjarrald
,
Ernani L. Nascimento
,
Meiry S. Sakamoto
,
Christopher Cunningham
,
Jean-Pierre Chaboureau
,
Walter A. Petersen
,
David K. Adams
,
Luca Baldini
,
Carlos F. Angelis
,
Luiz F. Sapucci
,
Paola Salio
,
Henrique M. J. Barbosa
,
Eduardo Landulfo
,
Rodrigo A. F. Souza
,
Richard J. Blakeslee
,
Jeffrey Bailey
,
Saulo Freitas
,
Wagner F. A. Lima
, and
Ali Tokay

CHUVA, meaning “rain” in Portuguese, is the acronym for the Cloud Processes of the Main Precipitation Systems in Brazil: A Contribution to Cloud-Resolving Modeling and to the Global Precipitation Measurement (GPM). The CHUVA project has conducted five field campaigns; the sixth and last campaign will be held in Manaus in 2014. The primary scientific objective of CHUVA is to contribute to the understanding of cloud processes, which represent one of the least understood components of the weather and climate system. The five CHUVA campaigns were designed to investigate specific tropical weather regimes. The first two experiments, in Alcantara and Fortaleza in northeastern Brazil, focused on warm clouds. The third campaign, which was conducted in Belém, was dedicated to tropical squall lines that often form along the sea-breeze front. The fourth campaign was in the Vale do Paraiba of southeastern Brazil, which is a region with intense lightning activity. In addition to contributing to the understanding of cloud process evolution from storms to thunderstorms, this fourth campaign also provided a high-fidelity total lightning proxy dataset for the NOAA Geostationary Operational Environmental Satellite (GOES)-R program. The fifth campaign was carried out in Santa Maria, in southern Brazil, a region of intense hailstorms associated with frequent mesoscale convective complexes. This campaign employed a multimodel high-resolution ensemble experiment. The data collected from contrasting precipitation regimes in tropical continental regions allow the various cloud processes in diverse environments to be compared. Some examples of these previous experiments are presented to illustrate the variability of convection across the tropics.

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Paola Salio
,
Hernán Bechis
,
Bruno Z. Ribeiro
,
Ernani de Lima Nascimento
,
Vito Galligani
,
Fernando Garcia
,
Lucas Alvarenga
,
Maria de los Milagros Alvarezs Imaz
,
Daiana Marlene Baissac
,
María Florencia Barle
,
Cristian Bastías-Curivil
,
Marcos Benedicto
,
Maite Cancelada
,
Izabelly Carvalho da Costa
,
Daniela D’Amen
,
Ramon de Elia
,
David Eduardo Diaz
,
Anthony Duarte Páez
,
Sergio González
,
Vitor Goede
,
Julián Goñi
,
Agustín Granato
,
Murilo Machado Lopes
,
Matias Mederos
,
Matias Menalled
,
Romina Mezher
,
Eduardo José Mingo Vega
,
María Gabriela Nicora
,
Lucía Pini
,
Roberto Rondanelli
,
Juan Jose Ruiz
,
Nestor Santayana
,
Laís Santos
,
Guilherme Schild
,
Inés Simone
,
Raul Valenzuela
,
Yasmin Romina Velazquez
,
Luciano Vidal
, and
Constanza Inés Villagrán Asiares

Abstract

Despite southern South America being recognized as a hotspot for deep convective storms, little is known about the socioenvironmental impacts of high-impact weather (HIW) events. Although there have been past efforts to collect severe weather reports in the region, they have been highly fragmented among and within countries, sharing no common protocol, and limited to a particular phenomenon, a very specific region, or a short period of time. There is a pressing need for a more comprehensive understanding of the present risks linked to HIW events, specifically deep convective storms, on a global scale as well as their variability and potential future evolution in the context of climate change. A database of high-quality and systematic HIW reports and associated socioenvironmental impacts is essential to understand the regional atmospheric conditions leading to hazardous weather, to quantify its predictability, and to build robust early warning systems. To tackle this problem and following successful initiatives in other regions of the world, researchers, national weather service members, and weather enthusiasts from Argentina, Brazil, Chile, Paraguay, and Uruguay have embarked on a multinational collaboration to generate a standardized database of reports of HIW events principally associated with convective storms and their socioenvironmental impacts in South America. The goal of this paper is to describe this unprecedented initiative over the region, to summarize first results, and to discuss the potential applications of this collaboration.

Open access
Stephen W. Nesbitt
,
Paola V. Salio
,
Eldo Ávila
,
Phillip Bitzer
,
Lawrence Carey
,
V. Chandrasekar
,
Wiebke Deierling
,
Francina Dominguez
,
Maria Eugenia Dillon
,
C. Marcelo Garcia
,
David Gochis
,
Steven Goodman
,
Deanna A. Hence
,
Karen A. Kosiba
,
Matthew R. Kumjian
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Timothy Lang
,
Lorena Medina Luna
,
James Marquis
,
Robert Marshall
,
Lynn A. McMurdie
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Ernani de Lima Nascimento
,
Kristen L. Rasmussen
,
Rita Roberts
,
Angela K. Rowe
,
Juan José Ruiz
,
Eliah F.M.T. São Sabbas
,
A. Celeste Saulo
,
Russ S. Schumacher
,
Yanina Garcia Skabar
,
Luiz Augusto Toledo Machado
,
Robert J. Trapp
,
Adam C. Varble
,
James Wilson
,
Joshua Wurman
,
Edward J. Zipser
,
Ivan Arias
,
Hernán Bechis
, and
Maxwell A. Grover

Abstract

This article provides an overview of the experimental design, execution, education and public outreach, data collection, and initial scientific results from the Remote Sensing of Electrification, Lightning, and Mesoscale/Microscale Processes with Adaptive Ground Observations (RELAMPAGO) field campaign. RELAMPAGO was a major field campaign conducted in the Córdoba and Mendoza provinces in Argentina and western Rio Grande do Sul State in Brazil in 2018–19 that involved more than 200 scientists and students from the United States, Argentina, and Brazil. This campaign was motivated by the physical processes and societal impacts of deep convection that frequently initiates in this region, often along the complex terrain of the Sierras de Córdoba and Andes, and often grows rapidly upscale into dangerous storms that impact society. Observed storms during the experiment produced copious hail, intense flash flooding, extreme lightning flash rates, and other unusual lightning phenomena, but few tornadoes. The five distinct scientific foci of RELAMPAGO—convection initiation, severe weather, upscale growth, hydrometeorology, and lightning and electrification—are described, as are the deployment strategies to observe physical processes relevant to these foci. The campaign’s international cooperation, forecasting efforts, and mission planning strategies enabled a successful data collection effort. In addition, the legacy of RELAMPAGO in South America, including extensive multinational education, public outreach, and social media data gathering associated with the campaign, is summarized.

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