EVALUACIÓN DE LOS PARÁMETROS DEL VIENTO EN LOS PERÍODOS DE LLUVIA Y SEQUÍA EN EL VALLE SUBMARINO DE ARAYA, VENEZUELA. I PARTE
Summary: Wind evaluation is fundamental for understanding our sea dynamics. Lack of meteorological information is acute and there are not systematic meteorological measures in extended regions of Venezuela northeastern area. The aim of these study is to describe wind parameters behavior in Araya und...
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ftdatacite:10.5281/zenodo.3975472 2023-05-15T17:36:58+02:00 EVALUACIÓN DE LOS PARÁMETROS DEL VIENTO EN LOS PERÍODOS DE LLUVIA Y SEQUÍA EN EL VALLE SUBMARINO DE ARAYA, VENEZUELA. I PARTE Quintero, Antonio Terejova, Galina 2016 https://dx.doi.org/10.5281/zenodo.3975472 https://zenodo.org/record/3975472 es spa Zenodo https://dx.doi.org/10.5281/zenodo.3975473 Open Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 info:eu-repo/semantics/openAccess CC-BY Araya peninsula, field wind, automatic weather station Caribbean Sea Text Journal article article-journal ScholarlyArticle 2016 ftdatacite https://doi.org/10.5281/zenodo.3975472 https://doi.org/10.5281/zenodo.3975473 2021-11-05T12:55:41Z Summary: Wind evaluation is fundamental for understanding our sea dynamics. Lack of meteorological information is acute and there are not systematic meteorological measures in extended regions of Venezuela northeastern area. The aim of these study is to describe wind parameters behavior in Araya underwater valley, in the frame of weather conditions of Caribbean region. In ordert to evaluate wind parameters, information was taken from an automatic Cambell CR 1000 meteorological station located at at 10 ° 38’ 2,8” Lat. N, 64 ° 02’ 57.7” Long. W, 35 meters above sea level. The information collected corresponds to February and March 2011 (dry season) and August and September of the same year (rainy season) and it consisted of time observations of speed and direction of wind. The field of winds of the South of the Caribbean Sea was related with high pressures in the North Atlantic dry season, showing speeds of 4.0 m/s - 5.0 m/s and the direction from the 1st quadrant extends in the low troposphere up to 3.0 km. In the rainy season, the anticyclone of Azores is weak and scattered, resulting even in two centers (Azores itself and Sargasso). In the rainy season, winds are less intense and decrease to 2.0 m/s - 3.0 m/s. The weakening of the anticyclone encourages the manifestation of other atmospheric structures and it altered the regime of trade winds. The above is supported in specific measurements, this way, the average speed of the wind in February and March was 5.1 m/s and 4.9 m/s, respectively (4.9 m/s). During this time, there are predominant winds with direction E-ENE 69.2% (40.2% and 29.0%, respectively). In August and September the wind speed decreased to 3.7 m/s and 3.4 m/s respectively (3.6 m/s). This season, the winds are more disperse and come from all possible directions. The reponderance of E winds decreased to 25.7% in August and 20.1% in September, while winds from ENE decreased 18.0% in August and 14.9% in September. Text North Atlantic DataCite Metadata Store (German National Library of Science and Technology) Del Viento ENVELOPE(-66.833,-66.833,-68.617,-68.617) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
Spanish |
topic |
Araya peninsula, field wind, automatic weather station Caribbean Sea |
spellingShingle |
Araya peninsula, field wind, automatic weather station Caribbean Sea Quintero, Antonio Terejova, Galina EVALUACIÓN DE LOS PARÁMETROS DEL VIENTO EN LOS PERÍODOS DE LLUVIA Y SEQUÍA EN EL VALLE SUBMARINO DE ARAYA, VENEZUELA. I PARTE |
topic_facet |
Araya peninsula, field wind, automatic weather station Caribbean Sea |
description |
Summary: Wind evaluation is fundamental for understanding our sea dynamics. Lack of meteorological information is acute and there are not systematic meteorological measures in extended regions of Venezuela northeastern area. The aim of these study is to describe wind parameters behavior in Araya underwater valley, in the frame of weather conditions of Caribbean region. In ordert to evaluate wind parameters, information was taken from an automatic Cambell CR 1000 meteorological station located at at 10 ° 38’ 2,8” Lat. N, 64 ° 02’ 57.7” Long. W, 35 meters above sea level. The information collected corresponds to February and March 2011 (dry season) and August and September of the same year (rainy season) and it consisted of time observations of speed and direction of wind. The field of winds of the South of the Caribbean Sea was related with high pressures in the North Atlantic dry season, showing speeds of 4.0 m/s - 5.0 m/s and the direction from the 1st quadrant extends in the low troposphere up to 3.0 km. In the rainy season, the anticyclone of Azores is weak and scattered, resulting even in two centers (Azores itself and Sargasso). In the rainy season, winds are less intense and decrease to 2.0 m/s - 3.0 m/s. The weakening of the anticyclone encourages the manifestation of other atmospheric structures and it altered the regime of trade winds. The above is supported in specific measurements, this way, the average speed of the wind in February and March was 5.1 m/s and 4.9 m/s, respectively (4.9 m/s). During this time, there are predominant winds with direction E-ENE 69.2% (40.2% and 29.0%, respectively). In August and September the wind speed decreased to 3.7 m/s and 3.4 m/s respectively (3.6 m/s). This season, the winds are more disperse and come from all possible directions. The reponderance of E winds decreased to 25.7% in August and 20.1% in September, while winds from ENE decreased 18.0% in August and 14.9% in September. |
format |
Text |
author |
Quintero, Antonio Terejova, Galina |
author_facet |
Quintero, Antonio Terejova, Galina |
author_sort |
Quintero, Antonio |
title |
EVALUACIÓN DE LOS PARÁMETROS DEL VIENTO EN LOS PERÍODOS DE LLUVIA Y SEQUÍA EN EL VALLE SUBMARINO DE ARAYA, VENEZUELA. I PARTE |
title_short |
EVALUACIÓN DE LOS PARÁMETROS DEL VIENTO EN LOS PERÍODOS DE LLUVIA Y SEQUÍA EN EL VALLE SUBMARINO DE ARAYA, VENEZUELA. I PARTE |
title_full |
EVALUACIÓN DE LOS PARÁMETROS DEL VIENTO EN LOS PERÍODOS DE LLUVIA Y SEQUÍA EN EL VALLE SUBMARINO DE ARAYA, VENEZUELA. I PARTE |
title_fullStr |
EVALUACIÓN DE LOS PARÁMETROS DEL VIENTO EN LOS PERÍODOS DE LLUVIA Y SEQUÍA EN EL VALLE SUBMARINO DE ARAYA, VENEZUELA. I PARTE |
title_full_unstemmed |
EVALUACIÓN DE LOS PARÁMETROS DEL VIENTO EN LOS PERÍODOS DE LLUVIA Y SEQUÍA EN EL VALLE SUBMARINO DE ARAYA, VENEZUELA. I PARTE |
title_sort |
evaluación de los parámetros del viento en los períodos de lluvia y sequía en el valle submarino de araya, venezuela. i parte |
publisher |
Zenodo |
publishDate |
2016 |
url |
https://dx.doi.org/10.5281/zenodo.3975472 https://zenodo.org/record/3975472 |
long_lat |
ENVELOPE(-66.833,-66.833,-68.617,-68.617) |
geographic |
Del Viento |
geographic_facet |
Del Viento |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
https://dx.doi.org/10.5281/zenodo.3975473 |
op_rights |
Open Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.5281/zenodo.3975472 https://doi.org/10.5281/zenodo.3975473 |
_version_ |
1766136635690319872 |