Early summer surface air temperature variability over Pakistan and the role of El Niño–Southern Oscillation teleconnections

Early summer (May–June) is the season where the surface air temperature (SAT) variability is largest and may result in extreme temperature conditions over Pakistan. Therefore, we analysed the early summer interannual SAT variability over Pakistan for the period 1981–2018 using observational dataset...

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Published inInternational journal of climatology Vol. 42; no. 11; pp. 5768 - 5784
Main Authors Rashid, Irfan Ur, Abid, Muhammad Adnan, Almazroui, Mansour, Kucharski, Fred, Hanif, Muhammad, Ali, Shaukat, Ismail, Muhammad
Format Journal Article
LanguageEnglish
Published Chichester, UK John Wiley & Sons, Ltd 01.09.2022
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Abstract Early summer (May–June) is the season where the surface air temperature (SAT) variability is largest and may result in extreme temperature conditions over Pakistan. Therefore, we analysed the early summer interannual SAT variability over Pakistan for the period 1981–2018 using observational dataset and model simulations. We noted that upper‐level anticyclonic circulation anomalies over Pakistan, which are associated with upper to the middle tropospheric descending motion, favour clear skies with an increase in net shortwave radiation that leads to extreme surface warming over the region. Moreover, the El Niño–Southern Oscillation (ENSO) based on Niño3.4 SST index is negatively associated with SAT anomalies over Pakistan. The cold ENSO phase favours the positive geopotential height anomalies due to the strengthening of the Walker circulation that enhance the sinking motion and result in less cloudiness leading to the extreme higher surface temperature conditions over Pakistan, while the opposite happens in the warm ENSO phase. Moreover, the Saudi‐KAU Atmospheric Global Climate Model (AGCM) simulated large‐scale patterns that are in good agreement with the observations. Sensitivity experiments with the AGCM confirm that cold SST anomalies in the ENSO region significantly favour above‐normal SAT anomalies over Pakistan, while the opposite happens in the warm ENSO phase. These results are important to understand and potentially predict regional heatwaves over the South Asian region, particularly over Pakistan. Early summer surface air temperature (SAT) over Pakistan is modulated by the upper‐level positive geopotential height anomalies. ENSO is negatively associated with SAT over Pakistan and favours higher temperatures during its La Niña phase.
AbstractList Early summer (May–June) is the season where the surface air temperature (SAT) variability is largest and may result in extreme temperature conditions over Pakistan. Therefore, we analysed the early summer interannual SAT variability over Pakistan for the period 1981–2018 using observational dataset and model simulations. We noted that upper‐level anticyclonic circulation anomalies over Pakistan, which are associated with upper to the middle tropospheric descending motion, favour clear skies with an increase in net shortwave radiation that leads to extreme surface warming over the region. Moreover, the El Niño–Southern Oscillation (ENSO) based on Niño3.4 SST index is negatively associated with SAT anomalies over Pakistan. The cold ENSO phase favours the positive geopotential height anomalies due to the strengthening of the Walker circulation that enhance the sinking motion and result in less cloudiness leading to the extreme higher surface temperature conditions over Pakistan, while the opposite happens in the warm ENSO phase. Moreover, the Saudi‐KAU Atmospheric Global Climate Model (AGCM) simulated large‐scale patterns that are in good agreement with the observations. Sensitivity experiments with the AGCM confirm that cold SST anomalies in the ENSO region significantly favour above‐normal SAT anomalies over Pakistan, while the opposite happens in the warm ENSO phase. These results are important to understand and potentially predict regional heatwaves over the South Asian region, particularly over Pakistan. Early summer surface air temperature (SAT) over Pakistan is modulated by the upper‐level positive geopotential height anomalies. ENSO is negatively associated with SAT over Pakistan and favours higher temperatures during its La Niña phase.
Early summer (May–June) is the season where the surface air temperature (SAT) variability is largest and may result in extreme temperature conditions over Pakistan. Therefore, we analysed the early summer interannual SAT variability over Pakistan for the period 1981–2018 using observational dataset and model simulations. We noted that upper‐level anticyclonic circulation anomalies over Pakistan, which are associated with upper to the middle tropospheric descending motion, favour clear skies with an increase in net shortwave radiation that leads to extreme surface warming over the region. Moreover, the El Niño–Southern Oscillation (ENSO) based on Niño3.4 SST index is negatively associated with SAT anomalies over Pakistan. The cold ENSO phase favours the positive geopotential height anomalies due to the strengthening of the Walker circulation that enhance the sinking motion and result in less cloudiness leading to the extreme higher surface temperature conditions over Pakistan, while the opposite happens in the warm ENSO phase. Moreover, the Saudi‐KAU Atmospheric Global Climate Model (AGCM) simulated large‐scale patterns that are in good agreement with the observations. Sensitivity experiments with the AGCM confirm that cold SST anomalies in the ENSO region significantly favour above‐normal SAT anomalies over Pakistan, while the opposite happens in the warm ENSO phase. These results are important to understand and potentially predict regional heatwaves over the South Asian region, particularly over Pakistan.
Abstract Early summer (May–June) is the season where the surface air temperature (SAT) variability is largest and may result in extreme temperature conditions over Pakistan. Therefore, we analysed the early summer interannual SAT variability over Pakistan for the period 1981–2018 using observational dataset and model simulations. We noted that upper‐level anticyclonic circulation anomalies over Pakistan, which are associated with upper to the middle tropospheric descending motion, favour clear skies with an increase in net shortwave radiation that leads to extreme surface warming over the region. Moreover, the El Niño–Southern Oscillation (ENSO) based on Niño3.4 SST index is negatively associated with SAT anomalies over Pakistan. The cold ENSO phase favours the positive geopotential height anomalies due to the strengthening of the Walker circulation that enhance the sinking motion and result in less cloudiness leading to the extreme higher surface temperature conditions over Pakistan, while the opposite happens in the warm ENSO phase. Moreover, the Saudi‐KAU Atmospheric Global Climate Model (AGCM) simulated large‐scale patterns that are in good agreement with the observations. Sensitivity experiments with the AGCM confirm that cold SST anomalies in the ENSO region significantly favour above‐normal SAT anomalies over Pakistan, while the opposite happens in the warm ENSO phase. These results are important to understand and potentially predict regional heatwaves over the South Asian region, particularly over Pakistan.
Author Hanif, Muhammad
Ismail, Muhammad
Rashid, Irfan Ur
Ali, Shaukat
Kucharski, Fred
Abid, Muhammad Adnan
Almazroui, Mansour
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Snippet Early summer (May–June) is the season where the surface air temperature (SAT) variability is largest and may result in extreme temperature conditions over...
Abstract Early summer (May–June) is the season where the surface air temperature (SAT) variability is largest and may result in extreme temperature conditions...
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crossref
wiley
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StartPage 5768
SubjectTerms Air temperature
Anomalies
Anticyclonic circulation
Circulation anomalies
Clear sky
Climate models
Cloud cover
Cloudiness
Dynamic height
early summer
El Nino
El Nino phenomena
El Nino-Southern Oscillation event
ENSO
Extreme values
Geopotential
Geopotential height
Global climate
Global climate models
Hadley circulation
Heat waves
Heatwaves
Height anomalies
Pakistan
Radiation
Sea surface
Sea surface temperature anomalies
Seasonal variations
Short wave radiation
Southern Oscillation
Summer
surface air temperature
Surface temperature
Surface-air temperature relationships
Temperature
Temperature extremes
Temperature variability
Variability
Walker circulation
Title Early summer surface air temperature variability over Pakistan and the role of El Niño–Southern Oscillation teleconnections
URI https://onlinelibrary.wiley.com/doi/abs/10.1002%2Fjoc.7560
https://www.proquest.com/docview/2709993517
Volume 42
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