Climate variability over the reef corridor of the southwestern Gulf of Mexico

Fuente: Redalyc
Salvato in:
Dettagli Bibliografici
Autore principale: José de Jesús Salas-Pérez
Natura: Artículo científico
Lingua:en
Pubblicazione: Universidad Nacional Autónoma de México 2020
Soggetti:
Accesso online:
Tags: Aggiungi Tag
Nessun Tag, puoi essere il primo ad aggiungerne!!
_version_ 1876446879669026816
author José de Jesús Salas-Pérez
author_facet José de Jesús Salas-Pérez
contents Climate variability over the reef corridor of the southwestern Gulf of Mexico José de Jesús Salas-Pérez Adán Guillermo Jordán-Garza David Salas-Monreal Biología long AMO signal ENSO signal extreme values Los Tuxtlas reefs Local and regional climate trends drive rates of change in coastal ecosystems. To better understand local climate, 35-year-long time series of air temperature, relative humidity and rainfall were analyzed along the reef corridor of the southwestern Gulf of Mexico. Data came from a climatological model and to assess its local performance, differences with in situ records were estimated when available. All three variables showed coherence with the record of the North Atlantic high-pressure system (also known as the Bermuda High) at similar times and periods between 4 to 8 and >10 years, evidencing the influence, at this regional scale, of El Niño Southern Oscillation (ENSO) and the Atlantic Multidecadal Oscillation (AMO). Positive and negative anomalies showed linear trends depicting an increase of warmer and moister events during a seasonal cli-matology at the reef corridor of the southwestern Gulf of Mexico and a relatively higher correlation (> 0.5) with the AMO mode. Return periods of extreme values varied between 5 and 10 years. In general, trends and extreme events showed similar patterns at a regional scale, but the increase in rainfall is expected to be larger near the central location of the study area. A higher frequency of extreme events could threaten local ecosystems and human populations; therefore, plans and actions at local scales of governance are needed to achieve preemptive climate adaptation. 2020 artículo científico 0187-6236 https://www.redalyc.org/articulo.oa?id=56572268003 https://www.redalyc.org/journal/565/56572268003/ https://www.redalyc.org/journal/565/56572268003/html/ https://www.redalyc.org/journal/565/56572268003/56572268003.epub https://www.redalyc.org/journal/565/56572268003/movil 10.20937/ATM.52730 en http://www.redalyc.org/revista.oa?id=565 Atmósfera application/pdf Universidad Nacional Autónoma de México Atmósfera (México) Num.2 Vol.33
format Artículo científico
id redalyc_56572268003
institution Redalyc
language en
publishDate 2020
publisher Universidad Nacional Autónoma de México
spellingShingle Climate variability over the reef corridor of the southwestern Gulf of Mexico
José de Jesús Salas-Pérez
Biología
long
AMO signal
ENSO signal
extreme values
Los Tuxtlas reefs
Climate variability over the reef corridor of the southwestern Gulf of Mexico José de Jesús Salas-Pérez Adán Guillermo Jordán-Garza David Salas-Monreal Biología long AMO signal ENSO signal extreme values Los Tuxtlas reefs Local and regional climate trends drive rates of change in coastal ecosystems. To better understand local climate, 35-year-long time series of air temperature, relative humidity and rainfall were analyzed along the reef corridor of the southwestern Gulf of Mexico. Data came from a climatological model and to assess its local performance, differences with in situ records were estimated when available. All three variables showed coherence with the record of the North Atlantic high-pressure system (also known as the Bermuda High) at similar times and periods between 4 to 8 and >10 years, evidencing the influence, at this regional scale, of El Niño Southern Oscillation (ENSO) and the Atlantic Multidecadal Oscillation (AMO). Positive and negative anomalies showed linear trends depicting an increase of warmer and moister events during a seasonal cli-matology at the reef corridor of the southwestern Gulf of Mexico and a relatively higher correlation (> 0.5) with the AMO mode. Return periods of extreme values varied between 5 and 10 years. In general, trends and extreme events showed similar patterns at a regional scale, but the increase in rainfall is expected to be larger near the central location of the study area. A higher frequency of extreme events could threaten local ecosystems and human populations; therefore, plans and actions at local scales of governance are needed to achieve preemptive climate adaptation. 2020 artículo científico 0187-6236 https://www.redalyc.org/articulo.oa?id=56572268003 https://www.redalyc.org/journal/565/56572268003/ https://www.redalyc.org/journal/565/56572268003/html/ https://www.redalyc.org/journal/565/56572268003/56572268003.epub https://www.redalyc.org/journal/565/56572268003/movil 10.20937/ATM.52730 en http://www.redalyc.org/revista.oa?id=565 Atmósfera application/pdf Universidad Nacional Autónoma de México Atmósfera (México) Num.2 Vol.33
title Climate variability over the reef corridor of the southwestern Gulf of Mexico
topic Biología
long
AMO signal
ENSO signal
extreme values
Los Tuxtlas reefs
url https://www.redalyc.org/articulo.oa?id=56572268003
https://www.redalyc.org/journal/565/56572268003/
https://www.redalyc.org/journal/565/56572268003/html/
https://www.redalyc.org/journal/565/56572268003/56572268003.epub
https://www.redalyc.org/journal/565/56572268003/movil