Re-examining the roles of surface heat flux and latent heat release in a “hurricane-like” polar low over the Barents Sea

Kolstad, Erik W.; Bracegirdle, Thomas J. ORCID: https://orcid.org/0000-0002-8868-4739; Zahn, Matthias. 2016 Re-examining the roles of surface heat flux and latent heat release in a “hurricane-like” polar low over the Barents Sea. Journal of Geophysical Research: Atmospheres, 121 (13). 7853-7867. https://doi.org/10.1002/2015JD024633

Before downloading, please read NORA policies.

Preview

Text Copyright American Geophysical Union Kolstad_et_al-2016-Journal_of_Geophysical_Research__Atmospheres.pdf - Published Version Download (4MB) | Preview

Abstract/Summary

Polar lows are intense mesoscale cyclones that occur at high latitudes in both hemispheres during winter. Their sometimes evidently convective nature, fueled by strong surface fluxes and with cloud-free centers, have led to some polar lows being referred to as “arctic hurricanes.” Idealized studies have shown that intensification by hurricane development mechanisms is theoretically possible in polar winter atmospheres, but the lack of observations and realistic simulations of actual polar lows have made it difficult to ascertain if this occurs in reality. Here the roles of surface heat fluxes and latent heat release in the development of a Barents Sea polar low, which in its cloud structures showed some similarities to hurricanes, are studied with an ensemble of sensitivity experiments, where latent heating and/or surface fluxes of sensible and latent heat were switched off before the polar low peaked in intensity. To ensure that the polar lows in the sensitivity runs did not track too far away from the actual environmental conditions, a technique known as spectral nudging was applied. This was shown to be crucial for enabling comparisons between the different model runs. The results presented here show that (1) no intensification occurred during the mature, postbaroclinic stage of the simulated polar low; (2) surface heat fluxes, i.e., air-sea interaction, were crucial processes both in order to attain the polar low's peak intensity during the baroclinic stage and to maintain its strength in the mature stage; and (3) latent heat release played a less important role than surface fluxes in both stages.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1002/2015JD024633
Programmes:	BAS Programmes > BAS Programmes 2015 > Atmosphere, Ice and Climate
ISSN:	2169897X
Additional Keywords:	Arctic, polar lows
Date made live:	19 Jul 2016 12:51 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/513995

Actions (login required)

View Item

Document Downloads

More statistics for this item...