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: Luís Beltrán (10393075), Diana Cristina Díaz (10393078)
Format: Dataset
Language:unknown
Published: 2020
Subjects:
Online Access:https://doi.org/10.6084/m9.figshare.14281996.v1
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spelling ftsmithonian:oai:figshare.com:article/14281996 2023-05-15T17:30:25+02:00 Influence of the Macroclimatic Oscillations in the Gachaneca River Basin Weather Patterns; Boyaca-Colombia Luís Beltrán (10393075) Diana Cristina Díaz (10393078) 2020-06-01T08:47:25Z https://doi.org/10.6084/m9.figshare.14281996.v1 unknown https://figshare.com/articles/dataset/Influence_of_the_Macroclimatic_Oscillations_in_the_Gachaneca_River_Basin_Weather_Patterns_Boyaca-Colombia/14281996 doi:10.6084/m9.figshare.14281996.v1 CC BY 4.0 CC-BY Meteorology climate variability El Niño Southern oscillation North Atlantic oscillation quasi-biennial oscillation water supply Dataset 2020 ftsmithonian https://doi.org/10.6084/m9.figshare.14281996.v1 2021-04-11T16:48:04Z 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 Unknown
institution Open Polar
collection Unknown
op_collection_id ftsmithonian
language unknown
topic Meteorology
climate variability
El Niño Southern oscillation
North Atlantic oscillation
quasi-biennial oscillation
water supply
spellingShingle Meteorology
climate variability
El Niño Southern oscillation
North Atlantic oscillation
quasi-biennial oscillation
water supply
Luís Beltrán (10393075)
Diana Cristina Díaz (10393078)
Influence of the Macroclimatic Oscillations in the Gachaneca River Basin Weather Patterns; Boyaca-Colombia
topic_facet Meteorology
climate variability
El Niño Southern oscillation
North Atlantic oscillation
quasi-biennial oscillation
water supply
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 Luís Beltrán (10393075)
Diana Cristina Díaz (10393078)
author_facet Luís Beltrán (10393075)
Diana Cristina Díaz (10393078)
author_sort Luís Beltrán (10393075)
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
publishDate 2020
url https://doi.org/10.6084/m9.figshare.14281996.v1
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation https://figshare.com/articles/dataset/Influence_of_the_Macroclimatic_Oscillations_in_the_Gachaneca_River_Basin_Weather_Patterns_Boyaca-Colombia/14281996
doi:10.6084/m9.figshare.14281996.v1
op_rights CC BY 4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.6084/m9.figshare.14281996.v1
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