Temporal and spatial behavior of temperature and precipitation during the canícula (midsummer drought) under El Niño conditions in central México

Relatively few studies have been performed about the onset, duration, and intensity of the canícula (midsummer drought) within central México in response to El Niño/Southern Oscillation (ENSO) events. The objective of our research is to assess the impact of the El Niño (EN) phase of ENSO upon air temperature (T), precipitation (PP), and drought index (DI = PP/T) during the canícula period. Daily air temperature and precipitation data from weather stations throughout central México are averaged for eight consecutive 10 (or 11)-day periods during the summers of 1960 through 1998. The data are grouped into seven climate regions according to specific precipitation criteria. Statistical comparisons between EN and neutral (N) years for the seven regions are made with pooled average T, PP and DI values from the summer. Results indicate that the EN phase significantly increases air temperatures within the wetter climate regions. The El Niño phase also increases summer precipitation within five of the regions, though not significantly. The added summer rainfall during El Niño phase does not reduce drought intensity with the exception of brief intervals within the wetter regions. Roughly, during EN and N years the canicula begins on July 11 and ends on August 31.

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Main Authors: PERALTA-HERNÁNDEZ,A. R, BARBA-MARTÍNEZ,L. R, MAGAÑA-RUEDA,V. O, MATTHIAS,A. D, LUNA-RUÍZ,J. J
Format: Digital revista
Language:English
Published: Universidad Nacional Autónoma de México, Centro de Ciencias de la Atmósfera 2008
Online Access:http://www.scielo.org.mx/scielo.php?script=sci_arttext&pid=S0187-62362008000300004
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spelling oai:scielo:S0187-623620080003000042009-05-20Temporal and spatial behavior of temperature and precipitation during the canícula (midsummer drought) under El Niño conditions in central MéxicoPERALTA-HERNÁNDEZ,A. RBARBA-MARTÍNEZ,L. RMAGAÑA-RUEDA,V. OMATTHIAS,A. DLUNA-RUÍZ,J. J Canícula midsummer drought El Niño precipitation temperature drought index Relatively few studies have been performed about the onset, duration, and intensity of the canícula (midsummer drought) within central México in response to El Niño/Southern Oscillation (ENSO) events. The objective of our research is to assess the impact of the El Niño (EN) phase of ENSO upon air temperature (T), precipitation (PP), and drought index (DI = PP/T) during the canícula period. Daily air temperature and precipitation data from weather stations throughout central México are averaged for eight consecutive 10 (or 11)-day periods during the summers of 1960 through 1998. The data are grouped into seven climate regions according to specific precipitation criteria. Statistical comparisons between EN and neutral (N) years for the seven regions are made with pooled average T, PP and DI values from the summer. Results indicate that the EN phase significantly increases air temperatures within the wetter climate regions. The El Niño phase also increases summer precipitation within five of the regions, though not significantly. The added summer rainfall during El Niño phase does not reduce drought intensity with the exception of brief intervals within the wetter regions. Roughly, during EN and N years the canicula begins on July 11 and ends on August 31.info:eu-repo/semantics/openAccessUniversidad Nacional Autónoma de México, Centro de Ciencias de la AtmósferaAtmósfera v.21 n.3 20082008-07-01info:eu-repo/semantics/articletext/htmlhttp://www.scielo.org.mx/scielo.php?script=sci_arttext&pid=S0187-62362008000300004en
institution SCIELO
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country México
countrycode MX
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language English
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author PERALTA-HERNÁNDEZ,A. R
BARBA-MARTÍNEZ,L. R
MAGAÑA-RUEDA,V. O
MATTHIAS,A. D
LUNA-RUÍZ,J. J
spellingShingle PERALTA-HERNÁNDEZ,A. R
BARBA-MARTÍNEZ,L. R
MAGAÑA-RUEDA,V. O
MATTHIAS,A. D
LUNA-RUÍZ,J. J
Temporal and spatial behavior of temperature and precipitation during the canícula (midsummer drought) under El Niño conditions in central México
author_facet PERALTA-HERNÁNDEZ,A. R
BARBA-MARTÍNEZ,L. R
MAGAÑA-RUEDA,V. O
MATTHIAS,A. D
LUNA-RUÍZ,J. J
author_sort PERALTA-HERNÁNDEZ,A. R
title Temporal and spatial behavior of temperature and precipitation during the canícula (midsummer drought) under El Niño conditions in central México
title_short Temporal and spatial behavior of temperature and precipitation during the canícula (midsummer drought) under El Niño conditions in central México
title_full Temporal and spatial behavior of temperature and precipitation during the canícula (midsummer drought) under El Niño conditions in central México
title_fullStr Temporal and spatial behavior of temperature and precipitation during the canícula (midsummer drought) under El Niño conditions in central México
title_full_unstemmed Temporal and spatial behavior of temperature and precipitation during the canícula (midsummer drought) under El Niño conditions in central México
title_sort temporal and spatial behavior of temperature and precipitation during the canícula (midsummer drought) under el niño conditions in central méxico
description Relatively few studies have been performed about the onset, duration, and intensity of the canícula (midsummer drought) within central México in response to El Niño/Southern Oscillation (ENSO) events. The objective of our research is to assess the impact of the El Niño (EN) phase of ENSO upon air temperature (T), precipitation (PP), and drought index (DI = PP/T) during the canícula period. Daily air temperature and precipitation data from weather stations throughout central México are averaged for eight consecutive 10 (or 11)-day periods during the summers of 1960 through 1998. The data are grouped into seven climate regions according to specific precipitation criteria. Statistical comparisons between EN and neutral (N) years for the seven regions are made with pooled average T, PP and DI values from the summer. Results indicate that the EN phase significantly increases air temperatures within the wetter climate regions. The El Niño phase also increases summer precipitation within five of the regions, though not significantly. The added summer rainfall during El Niño phase does not reduce drought intensity with the exception of brief intervals within the wetter regions. Roughly, during EN and N years the canicula begins on July 11 and ends on August 31.
publisher Universidad Nacional Autónoma de México, Centro de Ciencias de la Atmósfera
publishDate 2008
url http://www.scielo.org.mx/scielo.php?script=sci_arttext&pid=S0187-62362008000300004
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