@Article{PintoJśniorPint:2020:LiChRe,
author = "Pinto J{\'u}nior, Osmar and Pinto, Iara Regina Cardoso de
Almeida",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)}",
title = "Lightning changes in response to global warming in Rio de Janeiro,
Brazil",
journal = "American Journal of Climate Change",
year = "2020",
volume = "9",
number = "3",
pages = "266--273",
keywords = "Lightning, Global Change, Rio de Janeiro, Brazil.",
abstract = "Physical concepts based on the Clausius-Clapeyron relation and on
the thermodynamics and aerosol characteristics associated with
updrafts, global climate models assuming different
parametrizations and lightning-related output variables, and
lightning-related data (thunderstorm days) are being used to infer
the lightning incidence in a warmer planet, motivated by the
global warming observed. In all cases, there are many gaps to be
overcome making the lightning response to the global temperature
increase still unpredicted. Values from almost 0% (no increase) to
100% have been estimated, being 10% the most common value. While
the physical concepts address only part of the problem and the
global climate models need to make many simple assumptions,
lightning-relate data have strong time and space limitations. In
this context, any new evidence should be considered as an
important contribution to better understand how will be the
lightning incidence in the future. In this article, we described
new results about the occurrence of thunderstorms from 1850 to
2010 (a period of 160 years) in the city of Rio de Janeiro, in the
Southeast of Brazil. During this period thunderstorm days were
recorded in the same location, making this time series one of the
longest series of this type available worldwide. The data support
an increase of 21% in the mean annual thunderstorm days during the
period, while surface temperature increased by 0.6°C during the
period. Considering that the mean annual number of thunderstorm in
the beginning of this period was 29, we found an increase of one
thunderstorm day per 0.1°C of increase in the surface temperature.
Assuming that the number of lightning flashes per thunderstorm
remains approximately constant during the period, this number
corresponds to an increase in the lightning flash rate of
approximately 35% per °C of increase of temperature. In addition,
considering that the increase of the global temperature during the
period was almost the same that observed in Rio de Janeiro, we can
conclude that this increase in the lightning flash rate is due to
the global warming with no effect of urban activity. Finally, we
found that monthly thunderstorm days and monthly mean surface
temperature show a linear correlation with a coefficient of 0.9
along the period.",
doi = "10.4236/ajcc.2020.93017",
url = "http://dx.doi.org/10.4236/ajcc.2020.93017",
issn = "2167-9495 and 2167-9509",
language = "en",
targetfile = "pinto_lightning.pdf",
urlaccessdate = "27 abr. 2024"
}