Editorial Type:
Article
Article Type:
Research Article

Characteristics of Summer Airflow over the Antarctic Peninsula in Response to Recent Strengthening of Westerly Circumpolar Winds

Andrew Orr Centre for Polar Observation and Modelling, University College London, London, United Kingdom

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Gareth J. Marshall British Antarctic Survey, Natural Environment Research Council, Cambridge, United Kingdom

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Julian C. R. Hunt Centre for Polar Observation and Modelling, University College London, London, United Kingdom

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Joel Sommeria LEGI/Coriolis, Grenoble, France

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Chang-Gui Wang Department of Meteorology, University of Reading, Reading, United Kingdom

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Nicole P. M. van Lipzig Physical and Regional Geography Research Group, K. U. Leuven, Heverlee, Belgium

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Doug Cresswell Centre for Polar Observation and Modelling, University College London, London, United Kingdom

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John C. King British Antarctic Survey, Natural Environment Research Council, Cambridge, United Kingdom

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Print Publication:
01 Apr 2008
DOI:
https://doi.org/10.1175/2007JAS2498.1
Page(s):
1396–1413
Restricted access

Abstract

Summer near-surface temperatures over the northeast coast of the Antarctic Peninsula have increased by more than 2°C over the past 40 years, a temperature increase 3 times greater than that on the northwest coast. Recent analysis has shown a strong correlation between this striking warming trend and significant change in the summer Southern Hemisphere annular mode (SAM), which has resulted in greatly increased summer westerlies across the northern peninsula. It has been proposed that the strengthening westerlies have resulted in increased vertical deflection of relatively warm maritime air over the northern peninsula, contributing significantly to the observed warming and the recent collapse of northern sections of the Larsen Ice Shelf. In this study, laboratory and numerical modeling of airflow incident to the peninsula are employed to further understand this mechanism. It is shown that the effect of the strengthening westerlies has led to a distinct transition from a “blocked” regime to a “flow-over” regime, that is, confirmation of the proposed warming mechanism. The blocked regime is dominated by flow stagnation upstream (i.e., little vertical deflection) and consequent lateral deflection of flow along the western side of the peninsula. The flow-over regime is dominated by vertical deflection of mid/upper-level air over the peninsula, with strong downslope winds following closely to the leeward slope transporting this air (which warms adiabatically as it descends) to the near-surface of the northeast peninsula. The strong rotation typical of high latitudes considerably increases the flow over the peninsula, particularly strengthening it over the southern side (verified by aircraft measurements), suggesting that the warming trend is not solely confined to the northeast. Globally, flow regime transitions such as this may be responsible for other local climate variations.

** Current affiliation: ECMWF, Reading, United Kingdom

Corresponding author address: Dr. Andrew Orr, ECMWF, Shinfield Rd., Reading RG2 9AX, United Kingdom. Email: andrew.orr@ecmwf.int

Abstract

Summer near-surface temperatures over the northeast coast of the Antarctic Peninsula have increased by more than 2°C over the past 40 years, a temperature increase 3 times greater than that on the northwest coast. Recent analysis has shown a strong correlation between this striking warming trend and significant change in the summer Southern Hemisphere annular mode (SAM), which has resulted in greatly increased summer westerlies across the northern peninsula. It has been proposed that the strengthening westerlies have resulted in increased vertical deflection of relatively warm maritime air over the northern peninsula, contributing significantly to the observed warming and the recent collapse of northern sections of the Larsen Ice Shelf. In this study, laboratory and numerical modeling of airflow incident to the peninsula are employed to further understand this mechanism. It is shown that the effect of the strengthening westerlies has led to a distinct transition from a “blocked” regime to a “flow-over” regime, that is, confirmation of the proposed warming mechanism. The blocked regime is dominated by flow stagnation upstream (i.e., little vertical deflection) and consequent lateral deflection of flow along the western side of the peninsula. The flow-over regime is dominated by vertical deflection of mid/upper-level air over the peninsula, with strong downslope winds following closely to the leeward slope transporting this air (which warms adiabatically as it descends) to the near-surface of the northeast peninsula. The strong rotation typical of high latitudes considerably increases the flow over the peninsula, particularly strengthening it over the southern side (verified by aircraft measurements), suggesting that the warming trend is not solely confined to the northeast. Globally, flow regime transitions such as this may be responsible for other local climate variations.

** Current affiliation: ECMWF, Reading, United Kingdom

Corresponding author address: Dr. Andrew Orr, ECMWF, Shinfield Rd., Reading RG2 9AX, United Kingdom. Email: andrew.orr@ecmwf.int

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