Influence of the Macroclimatic Oscillations in the Gachaneca River Basin Weather Patterns; Boyaca-Colombia

Abstract To study the influence of macroclimatic oscillations in the Gachaneca river basin this work studies the variability of minimum and maximum temperature and standardized precipitation indices in the basin area between the years 1982 and 2015, and evaluated the relation among these variables w...

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Main Authors: Beltrán, Luís, Díaz, Diana Cristina
Format: Dataset
Language:unknown
Published: SciELO journals 2021
Subjects:
Online Access:https://dx.doi.org/10.6084/m9.figshare.14281996.v1
https://scielo.figshare.com/articles/dataset/Influence_of_the_Macroclimatic_Oscillations_in_the_Gachaneca_River_Basin_Weather_Patterns_Boyaca-Colombia/14281996/1
id ftdatacite:10.6084/m9.figshare.14281996.v1
record_format openpolar
spelling ftdatacite:10.6084/m9.figshare.14281996.v1 2023-05-15T17:33:34+02:00 Influence of the Macroclimatic Oscillations in the Gachaneca River Basin Weather Patterns; Boyaca-Colombia Beltrán, Luís Díaz, Diana Cristina 2021 https://dx.doi.org/10.6084/m9.figshare.14281996.v1 https://scielo.figshare.com/articles/dataset/Influence_of_the_Macroclimatic_Oscillations_in_the_Gachaneca_River_Basin_Weather_Patterns_Boyaca-Colombia/14281996/1 unknown SciELO journals https://dx.doi.org/10.1590/0102-7786351012 https://dx.doi.org/10.6084/m9.figshare.14281996 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY 40107 Meteorology FOS Earth and related environmental sciences dataset Dataset 2021 ftdatacite https://doi.org/10.6084/m9.figshare.14281996.v1 https://doi.org/10.1590/0102-7786351012 https://doi.org/10.6084/m9.figshare.14281996 2021-11-05T12:55:41Z Abstract To study the influence of macroclimatic oscillations in the Gachaneca river basin this work studies the variability of minimum and maximum temperature and standardized precipitation indices in the basin area between the years 1982 and 2015, and evaluated the relation among these variables with El Niño Southern Oscillation (ENSO), North Atlantic Oscillation (NAO), and Quasi-Biennial Oscillation (OCB) by canonical correlation analysis. The results reveal that percentages of variance explained by macroclimatic phenomena in December-February range between 34% and 38%, in March-May between 15% and 20%, in June-August between 15% and 25% and in September- November between 21% and 34%. The most influential phenomenon is ENSO, followed by NAO. During DEF the study area is more exposed to dry events that increase the risk of depletion of water resources due to the warm phase of ENSO. The NAO can indirectly reinforce or mitigate drought events due to its relationship with the magnitude of the trade winds and the variability of the tropical Atlantic that have an impact on the position of the ITCZ and the convective processes of the region. Dataset North Atlantic North Atlantic oscillation DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic 40107 Meteorology
FOS Earth and related environmental sciences
spellingShingle 40107 Meteorology
FOS Earth and related environmental sciences
Beltrán, Luís
Díaz, Diana Cristina
Influence of the Macroclimatic Oscillations in the Gachaneca River Basin Weather Patterns; Boyaca-Colombia
topic_facet 40107 Meteorology
FOS Earth and related environmental sciences
description Abstract To study the influence of macroclimatic oscillations in the Gachaneca river basin this work studies the variability of minimum and maximum temperature and standardized precipitation indices in the basin area between the years 1982 and 2015, and evaluated the relation among these variables with El Niño Southern Oscillation (ENSO), North Atlantic Oscillation (NAO), and Quasi-Biennial Oscillation (OCB) by canonical correlation analysis. The results reveal that percentages of variance explained by macroclimatic phenomena in December-February range between 34% and 38%, in March-May between 15% and 20%, in June-August between 15% and 25% and in September- November between 21% and 34%. The most influential phenomenon is ENSO, followed by NAO. During DEF the study area is more exposed to dry events that increase the risk of depletion of water resources due to the warm phase of ENSO. The NAO can indirectly reinforce or mitigate drought events due to its relationship with the magnitude of the trade winds and the variability of the tropical Atlantic that have an impact on the position of the ITCZ and the convective processes of the region.
format Dataset
author Beltrán, Luís
Díaz, Diana Cristina
author_facet Beltrán, Luís
Díaz, Diana Cristina
author_sort Beltrán, Luís
title Influence of the Macroclimatic Oscillations in the Gachaneca River Basin Weather Patterns; Boyaca-Colombia
title_short Influence of the Macroclimatic Oscillations in the Gachaneca River Basin Weather Patterns; Boyaca-Colombia
title_full Influence of the Macroclimatic Oscillations in the Gachaneca River Basin Weather Patterns; Boyaca-Colombia
title_fullStr Influence of the Macroclimatic Oscillations in the Gachaneca River Basin Weather Patterns; Boyaca-Colombia
title_full_unstemmed Influence of the Macroclimatic Oscillations in the Gachaneca River Basin Weather Patterns; Boyaca-Colombia
title_sort influence of the macroclimatic oscillations in the gachaneca river basin weather patterns; boyaca-colombia
publisher SciELO journals
publishDate 2021
url https://dx.doi.org/10.6084/m9.figshare.14281996.v1
https://scielo.figshare.com/articles/dataset/Influence_of_the_Macroclimatic_Oscillations_in_the_Gachaneca_River_Basin_Weather_Patterns_Boyaca-Colombia/14281996/1
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation https://dx.doi.org/10.1590/0102-7786351012
https://dx.doi.org/10.6084/m9.figshare.14281996
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.6084/m9.figshare.14281996.v1
https://doi.org/10.1590/0102-7786351012
https://doi.org/10.6084/m9.figshare.14281996
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