Multidecadal Variations in the Relationship between the NAO and Winter Precipitation in the Hindu Kush–Karakoram

Winter precipitation over the Hindu Kush–Karakoram (HKK) range in the western Himalayas is generated by westerly perturbations whose dynamics is affected by the North Atlantic Oscillation (NAO). Larger precipitation is typically recorded during the positive NAO phase. In this work, the relationship...

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Published in:Journal of Climate
Main Authors: Filippi, Luca, Palazzi, Elisa, von Hardenberg, Jost, Provenzale, Antonello
Language:unknown
Published: 2023
Subjects:
Online Access:http://www.osti.gov/servlets/purl/1565385
https://www.osti.gov/biblio/1565385
https://doi.org/10.1175/jcli-d-14-00286.1
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spelling ftosti:oai:osti.gov:1565385 2023-07-30T04:05:30+02:00 Multidecadal Variations in the Relationship between the NAO and Winter Precipitation in the Hindu Kush–Karakoram Filippi, Luca Palazzi, Elisa von Hardenberg, Jost Provenzale, Antonello 2023-06-23 application/pdf http://www.osti.gov/servlets/purl/1565385 https://www.osti.gov/biblio/1565385 https://doi.org/10.1175/jcli-d-14-00286.1 unknown http://www.osti.gov/servlets/purl/1565385 https://www.osti.gov/biblio/1565385 https://doi.org/10.1175/jcli-d-14-00286.1 doi:10.1175/jcli-d-14-00286.1 54 ENVIRONMENTAL SCIENCES 2023 ftosti https://doi.org/10.1175/jcli-d-14-00286.1 2023-07-11T09:37:06Z Winter precipitation over the Hindu Kush–Karakoram (HKK) range in the western Himalayas is generated by westerly perturbations whose dynamics is affected by the North Atlantic Oscillation (NAO). Larger precipitation is typically recorded during the positive NAO phase. In this work, the relationship between the NAO and winter precipitation in the HKK is explored further, using an ensemble of precipitation datasets and the 40-yr ECMWF Re-Analysis (ERA-40) and Twentieth Century Reanalysis (20CR) data. The mechanisms underlying this relationship are discussed, with a focus on the secular variations that occurred in the last century. The NAO exerts its control on HKK precipitation by altering the intensity of westerly winds in the region of the Middle East jet stream (MEJS). Results indicate that evaporation from the Persian Gulf, the northern Arabian Sea, and the Red Sea plays an important role. During positive NAO phases, westerlies are strengthened and enhanced evaporation occurs from these basins owing to higher surface wind speed. The extra moisture combines with stronger westerlies and results in enhanced moisture transport toward the HKK. Precipitation datasets covering the twentieth century show an alternation of periods of strong and weaker influence of the NAO on precipitation in the HKK. It is found that these variations are associated with changes in the spatial pattern of the NAO: the relative position of the two centers of action of the NAO determines to what extent it can modulate the MEJS, affecting precipitation in the HKK. Other/Unknown Material North Atlantic North Atlantic oscillation SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Journal of Climate 27 20 7890 7902
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 54 ENVIRONMENTAL SCIENCES
spellingShingle 54 ENVIRONMENTAL SCIENCES
Filippi, Luca
Palazzi, Elisa
von Hardenberg, Jost
Provenzale, Antonello
Multidecadal Variations in the Relationship between the NAO and Winter Precipitation in the Hindu Kush–Karakoram
topic_facet 54 ENVIRONMENTAL SCIENCES
description Winter precipitation over the Hindu Kush–Karakoram (HKK) range in the western Himalayas is generated by westerly perturbations whose dynamics is affected by the North Atlantic Oscillation (NAO). Larger precipitation is typically recorded during the positive NAO phase. In this work, the relationship between the NAO and winter precipitation in the HKK is explored further, using an ensemble of precipitation datasets and the 40-yr ECMWF Re-Analysis (ERA-40) and Twentieth Century Reanalysis (20CR) data. The mechanisms underlying this relationship are discussed, with a focus on the secular variations that occurred in the last century. The NAO exerts its control on HKK precipitation by altering the intensity of westerly winds in the region of the Middle East jet stream (MEJS). Results indicate that evaporation from the Persian Gulf, the northern Arabian Sea, and the Red Sea plays an important role. During positive NAO phases, westerlies are strengthened and enhanced evaporation occurs from these basins owing to higher surface wind speed. The extra moisture combines with stronger westerlies and results in enhanced moisture transport toward the HKK. Precipitation datasets covering the twentieth century show an alternation of periods of strong and weaker influence of the NAO on precipitation in the HKK. It is found that these variations are associated with changes in the spatial pattern of the NAO: the relative position of the two centers of action of the NAO determines to what extent it can modulate the MEJS, affecting precipitation in the HKK.
author Filippi, Luca
Palazzi, Elisa
von Hardenberg, Jost
Provenzale, Antonello
author_facet Filippi, Luca
Palazzi, Elisa
von Hardenberg, Jost
Provenzale, Antonello
author_sort Filippi, Luca
title Multidecadal Variations in the Relationship between the NAO and Winter Precipitation in the Hindu Kush–Karakoram
title_short Multidecadal Variations in the Relationship between the NAO and Winter Precipitation in the Hindu Kush–Karakoram
title_full Multidecadal Variations in the Relationship between the NAO and Winter Precipitation in the Hindu Kush–Karakoram
title_fullStr Multidecadal Variations in the Relationship between the NAO and Winter Precipitation in the Hindu Kush–Karakoram
title_full_unstemmed Multidecadal Variations in the Relationship between the NAO and Winter Precipitation in the Hindu Kush–Karakoram
title_sort multidecadal variations in the relationship between the nao and winter precipitation in the hindu kush–karakoram
publishDate 2023
url http://www.osti.gov/servlets/purl/1565385
https://www.osti.gov/biblio/1565385
https://doi.org/10.1175/jcli-d-14-00286.1
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation http://www.osti.gov/servlets/purl/1565385
https://www.osti.gov/biblio/1565385
https://doi.org/10.1175/jcli-d-14-00286.1
doi:10.1175/jcli-d-14-00286.1
op_doi https://doi.org/10.1175/jcli-d-14-00286.1
container_title Journal of Climate
container_volume 27
container_issue 20
container_start_page 7890
op_container_end_page 7902
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