Spatio-Temporal Distribution of Deep Convection Observed along the Trans-Mexican Volcanic Belt

Complex terrain features—in particular, environmental conditions, high population density and potential socio-economic damage—make the Trans-Mexican Volcanic Belt (TMVB) of particular interest regarding the study of deep convection and related severe weather. In this research, 10 years of Moderate-R...

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Main Authors: José Francisco León-Cruz, Cintia Carbajal Henken, Noel Carbajal, Jürgen Fischer
Format: Article
Language:English
Published: MDPI AG 2021-03-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/13/6/1215
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spelling doaj-2dd2261a5b834726b026ddbea7b135812021-03-24T00:04:32ZengMDPI AGRemote Sensing2072-42922021-03-01131215121510.3390/rs13061215Spatio-Temporal Distribution of Deep Convection Observed along the Trans-Mexican Volcanic BeltJosé Francisco León-Cruz0Cintia Carbajal Henken1Noel Carbajal2Jürgen Fischer3Departamento de Geografía Física, Instituto de Geografía, Universidad Nacional Autónoma de México (UNAM), Circuito de la Investigación Científica, Ciudad Universitaria, Coyoacán 04510, MexicoInstitute for Space Sciences, Freie Universität Berlin (FUB), Carl-Heinrich-Becker-Weg 6-10, 12165 Berlin, GermanyDivisión de Geociencias Aplicadas, Instituto Potosino de Investigación Científica y Tecnológica A.C. (IPICYT), Camino a la Presa de San José 2055, Lomas 4ta Secc, San Luis Potosí 78216, MexicoInstitute for Space Sciences, Freie Universität Berlin (FUB), Carl-Heinrich-Becker-Weg 6-10, 12165 Berlin, GermanyComplex terrain features—in particular, environmental conditions, high population density and potential socio-economic damage—make the Trans-Mexican Volcanic Belt (TMVB) of particular interest regarding the study of deep convection and related severe weather. In this research, 10 years of Moderate-Resolution Imaging Spectroradiometer (MODIS) cloud observations are combined with Climate Hazards Group Infrared Precipitation with Station (CHIRPS) rainfall data to characterize the spatio-temporal distribution of deep convective clouds (DCCs) and their relationship to extreme precipitation. From monthly distributions, wet and dry phases are identified for cloud fraction, deep convective cloud frequency and convective precipitation. For both DCC and extreme precipitation events, the highest frequencies align just over the higher elevations of the TMVB. A clear relationship between DCCs and terrain features, indicating the important role of orography in the development of convective systems, is noticed. For three sub-regions, the observed distributions of deep convective cloud and extreme precipitation events are assessed in more detail. Each sub-region exhibits different local conditions, including terrain features, and are known to be influenced differently by emerging moisture fluxes from the Gulf of Mexico and the Pacific Ocean. The observed distinct spatio-temporal variabilities provide the first insights into the physical processes that control the convective development in the study area. A signal of the midsummer drought in Mexico (i.e., “canícula”) is recognized using MODIS monthly mean cloud observations.https://www.mdpi.com/2072-4292/13/6/1215deep convectionassociated severe weatherprecipitationcomplex terrainMODISCHIRPS
collection DOAJ
language English
format Article
sources DOAJ
author José Francisco León-Cruz
Cintia Carbajal Henken
Noel Carbajal
Jürgen Fischer
spellingShingle José Francisco León-Cruz
Cintia Carbajal Henken
Noel Carbajal
Jürgen Fischer
Spatio-Temporal Distribution of Deep Convection Observed along the Trans-Mexican Volcanic Belt
Remote Sensing
deep convection
associated severe weather
precipitation
complex terrain
MODIS
CHIRPS
author_facet José Francisco León-Cruz
Cintia Carbajal Henken
Noel Carbajal
Jürgen Fischer
author_sort José Francisco León-Cruz
title Spatio-Temporal Distribution of Deep Convection Observed along the Trans-Mexican Volcanic Belt
title_short Spatio-Temporal Distribution of Deep Convection Observed along the Trans-Mexican Volcanic Belt
title_full Spatio-Temporal Distribution of Deep Convection Observed along the Trans-Mexican Volcanic Belt
title_fullStr Spatio-Temporal Distribution of Deep Convection Observed along the Trans-Mexican Volcanic Belt
title_full_unstemmed Spatio-Temporal Distribution of Deep Convection Observed along the Trans-Mexican Volcanic Belt
title_sort spatio-temporal distribution of deep convection observed along the trans-mexican volcanic belt
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2021-03-01
description Complex terrain features—in particular, environmental conditions, high population density and potential socio-economic damage—make the Trans-Mexican Volcanic Belt (TMVB) of particular interest regarding the study of deep convection and related severe weather. In this research, 10 years of Moderate-Resolution Imaging Spectroradiometer (MODIS) cloud observations are combined with Climate Hazards Group Infrared Precipitation with Station (CHIRPS) rainfall data to characterize the spatio-temporal distribution of deep convective clouds (DCCs) and their relationship to extreme precipitation. From monthly distributions, wet and dry phases are identified for cloud fraction, deep convective cloud frequency and convective precipitation. For both DCC and extreme precipitation events, the highest frequencies align just over the higher elevations of the TMVB. A clear relationship between DCCs and terrain features, indicating the important role of orography in the development of convective systems, is noticed. For three sub-regions, the observed distributions of deep convective cloud and extreme precipitation events are assessed in more detail. Each sub-region exhibits different local conditions, including terrain features, and are known to be influenced differently by emerging moisture fluxes from the Gulf of Mexico and the Pacific Ocean. The observed distinct spatio-temporal variabilities provide the first insights into the physical processes that control the convective development in the study area. A signal of the midsummer drought in Mexico (i.e., “canícula”) is recognized using MODIS monthly mean cloud observations.
topic deep convection
associated severe weather
precipitation
complex terrain
MODIS
CHIRPS
url https://www.mdpi.com/2072-4292/13/6/1215
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AT noelcarbajal spatiotemporaldistributionofdeepconvectionobservedalongthetransmexicanvolcanicbelt
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