The Telecommunications between Iraq Region Air Temperature and ENSO El NIÑO 3.4 Region

Background: El NIÑO phenomenon is a global climate phenomenon that occurs as a result of the interaction between the surface of the Pacific Ocean and the atmosphere directly above it. Objective: This study investigates whether El NIÑO 3.4 affects some of the climatic parameters in some Iraqi cities. Methods: A record surface data (2007-2017) of relative humidity, maximum and minimum air temperature was used from the Iraqi meteorological and seismology organization for seven selected meteorological stations, sea surface temperature anomalies from the royal Netherlands meteorological institute, and the reanalysis data of air temperature (1980-2022) from the national centers for environmental prediction and national center for atmospheric research. The climatic parameters data for seasonal and mean monthly are analyzed to understand the general trend, and the statistical relationships are investigated. Results: The result shows a decrease in relative humidity for Kirkuk and Nasiriya stations. Also, there is an increase in the general trend of the maximum and minimum temperatures for Kirkuk, Nasiriya, Basra, Baghdad, Al-Hay, and Mosul stations. The influence of the NIÑO 3.4 index on Iraq's climate, temperature, and relative humidity was minimal. The impact of the NIÑO 3.4 index on the maximum and minimum temperatures within the daily and monthly values, in general, was a weak positive correlation. The correlation between the NIÑO 3.4 index and the maximum and minimum temperatures during the spring and winter seasons is positive, while it is a negative correlation in the summer and autumn seasons. Conclusions: The main conclusion illustrated that the effect of the NIÑO 3.4 has a limited impact on the surface values of relative humidity and maximum and minimum air temperatures because there is a lag time in the response when the change of sea surface temperature anomalies starts to happen; it takes a month or more time until its impacts reach Iraq.

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Publication Details

Journal
Al-Mustansiriyah Journal of Science
Published
2025-03-30
DOI
https://doi.org/10.23851/mjs.v36i1.1558
Citations
1
Primary Topic
Climate variability and models
Type
article
Field-Weighted Citation Impact
1.11

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article

The Telecommunications between Iraq Region Air Temperature and ENSO El NIÑO 3.4 Region

Arjuna Castrillon, Ali Raheem Al‐Nassar, Muthanna A. Al-Tameemi, Aqeel Ghazi Mutar
1 citations
Al-Mustansiriyah Journal of Science
Climate variability and models
1.11
article

The Telecommunications between Iraq Region Air Temperature and ENSO El NIÑO 3.4 Region

Arjuna Castrillon, Ali Raheem Al‐Nassar, Muthanna A. Al-Tameemi, Aqeel Ghazi Mutar
article en
1 citations

Abstract

Background: El NIÑO phenomenon is a global climate phenomenon that occurs as a result of the interaction between the surface of the Pacific Ocean and the atmosphere directly above it. Objective: This study investigates whether El NIÑO 3.4 affects some of the climatic parameters in some Iraqi cities. Methods: A record surface data (2007-2017) of relative humidity, maximum and minimum air temperature was used from the Iraqi meteorological and seismology organization for seven selected meteorological stations, sea surface temperature anomalies from the royal Netherlands meteorological institute, and the reanalysis data of air temperature (1980-2022) from the national centers for environmental prediction and national center for atmospheric research. The climatic parameters data for seasonal and mean monthly are analyzed to understand the general trend, and the statistical relationships are investigated. Results: The result shows a decrease in relative humidity for Kirkuk and Nasiriya stations. Also, there is an increase in the general trend of the maximum and minimum temperatures for Kirkuk, Nasiriya, Basra, Baghdad, Al-Hay, and Mosul stations. The influence of the NIÑO 3.4 index on Iraq's climate, temperature, and relative humidity was minimal. The impact of the NIÑO 3.4 index on the maximum and minimum temperatures within the daily and monthly values, in general, was a weak positive correlation. The correlation between the NIÑO 3.4 index and the maximum and minimum temperatures during the spring and winter seasons is positive, while it is a negative correlation in the summer and autumn seasons. Conclusions: The main conclusion illustrated that the effect of the NIÑO 3.4 has a limited impact on the surface values of relative humidity and maximum and minimum air temperatures because there is a lag time in the response when the change of sea surface temperature anomalies starts to happen; it takes a month or more time until its impacts reach Iraq.

Al-Mustansiriyah Journal of ScienceVol. 36(1)
Mustansiriyah University (IQ), Colombian Geological Survey (CO)
National Oceanic and Atmospheric Administration
Openalex Percentile: Top 26%
Climate variability and models
1.11
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