Effect of Various Types of ENSO Events on Moisture Conditions in the Humid and Subhumid Tropics

Moisture anomaly conditions within humid and subhumid tropics that are associated with different types of El Niño and La Niña phenomena are described and analyzed with a focus on their spatial distribution and seasonal variability. Five dryness indices (Keetch–Byram Drought Index, Weighted Anomaly S...

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Main Authors: Daria Gushchina, Irina Zheleznova, Alexander Osipov, Alexander Olchev
Format: Article
Language:English
Published: MDPI AG 2020-12-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/11/12/1354
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author Daria Gushchina
Irina Zheleznova
Alexander Osipov
Alexander Olchev
author_facet Daria Gushchina
Irina Zheleznova
Alexander Osipov
Alexander Olchev
author_sort Daria Gushchina
collection DOAJ
description Moisture anomaly conditions within humid and subhumid tropics that are associated with different types of El Niño and La Niña phenomena are described and analyzed with a focus on their spatial distribution and seasonal variability. Five dryness indices (Keetch–Byram Drought Index, Weighted Anomaly Standardized Precipitation Index, Standardized Precipitation Index, Palmer Drought Severity Index, and Percent of Normal Precipitation) were derived from ECMWF (European Centre for Medium-Range Weather Forecasts) fifth generation reanalysis (ERA5) reanalysis and University Corporation for Atmospheric Research (UCAR) datasets for the period from 1979 to 2019. Cross-correlation analysis was used to evaluate the relationships between the El Niño Southern Oscillation (ENSO) and selected dryness indices. To describe the seasonal variability of the ENSO–surface moisture relationships, the composite maps of dryness indices in different seasons were analyzed. The results showed a significant heterogeneity of the ENSO-induced moisture anomaly conditions both within and across various geographical regions. Four main areas in humid and subhumid tropics with the maximum effects of El Niño/La Niña events on the surface moisture conditions were found: Southeast Asia and Australia, Eastern and South Africa, Northeastern and Eastern South America, and Central America. It was shown that the effects of La Niña were usually opposite to those of El Niño, while the responses to the two types of El Niño differed mostly in the moisture anomaly intensity and its spatial patterns.
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spelling doaj.art-409789e36d1c443a8d784156cd36093b2023-11-21T00:36:27ZengMDPI AGAtmosphere2073-44332020-12-011112135410.3390/atmos11121354Effect of Various Types of ENSO Events on Moisture Conditions in the Humid and Subhumid TropicsDaria Gushchina0Irina Zheleznova1Alexander Osipov2Alexander Olchev3Department of Meteorology and Climatology, Faculty of Geography, Lomonosov Moscow State University, GSP-1, Leninskie Gory, 119991 Moscow, RussiaDepartment of Meteorology and Climatology, Faculty of Geography, Lomonosov Moscow State University, GSP-1, Leninskie Gory, 119991 Moscow, RussiaDepartment of Meteorology and Climatology, Faculty of Geography, Lomonosov Moscow State University, GSP-1, Leninskie Gory, 119991 Moscow, RussiaDepartment of Meteorology and Climatology, Faculty of Geography, Lomonosov Moscow State University, GSP-1, Leninskie Gory, 119991 Moscow, RussiaMoisture anomaly conditions within humid and subhumid tropics that are associated with different types of El Niño and La Niña phenomena are described and analyzed with a focus on their spatial distribution and seasonal variability. Five dryness indices (Keetch–Byram Drought Index, Weighted Anomaly Standardized Precipitation Index, Standardized Precipitation Index, Palmer Drought Severity Index, and Percent of Normal Precipitation) were derived from ECMWF (European Centre for Medium-Range Weather Forecasts) fifth generation reanalysis (ERA5) reanalysis and University Corporation for Atmospheric Research (UCAR) datasets for the period from 1979 to 2019. Cross-correlation analysis was used to evaluate the relationships between the El Niño Southern Oscillation (ENSO) and selected dryness indices. To describe the seasonal variability of the ENSO–surface moisture relationships, the composite maps of dryness indices in different seasons were analyzed. The results showed a significant heterogeneity of the ENSO-induced moisture anomaly conditions both within and across various geographical regions. Four main areas in humid and subhumid tropics with the maximum effects of El Niño/La Niña events on the surface moisture conditions were found: Southeast Asia and Australia, Eastern and South Africa, Northeastern and Eastern South America, and Central America. It was shown that the effects of La Niña were usually opposite to those of El Niño, while the responses to the two types of El Niño differed mostly in the moisture anomaly intensity and its spatial patterns.https://www.mdpi.com/2073-4433/11/12/1354El Niño Southern Oscillationhumid and subhumid tropicsmoisture conditionsdryness indicesprecipitation anomalies
spellingShingle Daria Gushchina
Irina Zheleznova
Alexander Osipov
Alexander Olchev
Effect of Various Types of ENSO Events on Moisture Conditions in the Humid and Subhumid Tropics
Atmosphere
El Niño Southern Oscillation
humid and subhumid tropics
moisture conditions
dryness indices
precipitation anomalies
title Effect of Various Types of ENSO Events on Moisture Conditions in the Humid and Subhumid Tropics
title_full Effect of Various Types of ENSO Events on Moisture Conditions in the Humid and Subhumid Tropics
title_fullStr Effect of Various Types of ENSO Events on Moisture Conditions in the Humid and Subhumid Tropics
title_full_unstemmed Effect of Various Types of ENSO Events on Moisture Conditions in the Humid and Subhumid Tropics
title_short Effect of Various Types of ENSO Events on Moisture Conditions in the Humid and Subhumid Tropics
title_sort effect of various types of enso events on moisture conditions in the humid and subhumid tropics
topic El Niño Southern Oscillation
humid and subhumid tropics
moisture conditions
dryness indices
precipitation anomalies
url https://www.mdpi.com/2073-4433/11/12/1354
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