Hola amigos: A VUELO DE UN QUINDE EL BLOG., hemos recibido información de la Agencia Espacial NASA, que sus satélites han detectado que el aumento de precipitaciones pluviales en las zonas tropicales se debe a la aparición de las frecuentes grandes tormentas: Un nuevo estudio basado en parte en los datos de satélite de la NASA ha demostrado que un aumento en las grandes tormentas, bien organizados se incrementó tras las lluvias en las regiones más húmedas de los trópicos.
Muchos científicos han pensado durante mucho tiempo que, en un mundo en calentamiento algunas regiones es probable que veamos más lluvia porque una atmósfera más cálida es capaz de contener más vapor de agua. La idea parecía ser apoyada por observaciones recientes que muestran fuertes aumentos de precipitación en las regiones tropicales húmedas, que se refiere a veces como un patrón "rico-conseguir-ricos '.
Muchos científicos han pensado durante mucho tiempo que, en un mundo en calentamiento algunas regiones es probable que veamos más lluvia porque una atmósfera más cálida es capaz de contener más vapor de agua. La idea parecía ser apoyada por observaciones recientes que muestran fuertes aumentos de precipitación en las regiones tropicales húmedas, que se refiere a veces como un patrón "rico-conseguir-ricos '.
More information.............
A new study based in part on NASA satellite data has shown that an increase
in large, well-organized thunderstorms is behind increased rainfall in the
wettest regions of the tropics.
Many scientists have long thought that in a warming world some regions are
likely to see more rain because a warmer atmosphere is capable of holding more
water vapor. The idea seemed to be supported by recent observations showing
strong precipitation increases in the wettest tropical regions, sometimes
referred to as a 'rich-get-richer' pattern.
Joint research from the Australian
Research Council Centre of Excellence for Climate System Science (ARCCSS) and
NASA published online in Nature today reveals that rainfall increases
seen in places such as the western Pacific in recent decades are actually due to
large storms – what the authors call “organized deep convection” – happening
more frequently, rather than from individual storms producing more rain.
"The observations showed the increase in rainfall is directly caused by the
change in the character of rain events in the tropics rather than a change in
the total number of rain events," said lead author Jackson Tan, who conducted
this research while at Australia’s Monash University but now works at NASA’s
Wallops Flight Facility, Wallops Island, Virginia. "What we are seeing is more
big and organized storms and fewer small and disorganized rain events."
The
study helps chip away at one of the big questions facing climate change science:
To what degree will a warmer world accelerate the water cycle and patterns of
rainfall and drought? In particular, this study revolves around what scientists
call organized deep convection – in short, large thunderstorms. These storms
make up about five percent of the weather systems in the tropics but are
responsible for about 50 percent of tropical rainfall.
While this study does not delve into what’s causing the increase in large
storms, it does reveal a tight correlation between this trend and increasing
rainfall.
Analyzing rainfall and cloud data from 1983 to 2009, Tan found that these
large storms are still producing similar or even less amounts of rain on
average, but they are happening more often.
Tan began his research wanting to follow up on previous studies that showed
some regions of the tropics have experienced increased rainfall in recent
decades. Climate models predicted this would occur in a warming world.
“We are looking at what’s driving the changes in rainfall, and we are putting
another piece of the puzzle out there,” Tan said. “Frequency of organized deep
convection is definitely a part of this.”
Co-author George Tselioudis, a researcher at the NASA Goddard Institute for
Space Studies in New York, authored a paper in 2010 that defined trends in
organized deep convection in the tropics and sparked Tan’s curiosity on what was
driving those trends.
“This work changes our perception of why tropical precipitation is
increasing,” Tselioudis said. “We thought it was because the warmer atmosphere
holds more moisture and, therefore, when storms occur they rain more. But that
doesn’t seem to be the case. Instead, the warmer tropical atmosphere becomes
better organized to produce large storms more frequently.”
The researchers analyzed rainfall data from NASA’s Tropical Rainfall
Measuring Mission (from 1998-2009) and from the Global Precipitation Climatology
Project (from 1983-2009). These rainfall data were compared to cloud data from
the International Satellite Cloud Climatology Project for the period from 1983
to 2009.
While climate models have long predicted that a warmer world would see an
acceleration of the water cycle and changes in rainfall patterns, models have
not as of yet produced this change in the frequency of organized deep
convection.
The new finding also raises an intriguing next question: Why are these
weather systems organizing in the atmosphere more frequently? That’s not yet
known, Tan and Tselioudis said.
However, the finding does point the way to a new line of research on the
topic, Tselioudis said. Scientists have been focusing on the transfer of heat
and moisture in the atmosphere – the thermodynamics of the system. Tselioudis
said this finding should direct attention to the dynamics of the atmosphere –
the fundamental physics of circulation.
“For me, it’s high time we push in this direction,” Tselioudis said. “We’ve
been looking at the water cycle as if it’s mostly a thermodynamic issue. Just
being wet doesn’t rain make. There has to be more emphasis on the dynamics. If
you look at the grand challenges of figuring out the water cycle – this is where
the emphasis is moving to.”
Leslie McCarthy
Goddard Institute for Space Studies, New York
212-678-5507
leslie.m.mccarthy@nasa.gov
Goddard Institute for Space Studies, New York
212-678-5507
leslie.m.mccarthy@nasa.gov
NASA
Guillermo Gonzalo Sánchez Achutegui
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