elib
DLR-Header
DLR-Logo -> http://www.dlr.de
DLR Portal Home | Imprint | Privacy Policy | Contact | Deutsch
Fontsize: [-] Text [+]

On ice supersaturation over the Arctic

Gierens, Klaus Martin and Wilhelm, Lena and Sommer, Michael and Weaver, Dan (2020) On ice supersaturation over the Arctic. Meteorologische Zeitschrift, pp. 1-12. Borntraeger Science Publishers. doi: 10.1127/metz/2020/1012. ISSN 0941-2948.

[img] PDF - Postprint version (accepted manuscript)
2MB

Official URL: https://www.schweizerbart.de/papers/metz/detail/prepub/93340/On_ice_supersaturation_over_the_Arctic

Abstract

We study ice-supersaturation in the cold (<-38°C) arctic troposphere and lower stratosphere using high-resolution quality-controlled radiosonde data. On average, ice supersaturation occurs in about 40 % to 60 % of the profiles with frequency of occurrence increasing with geographic latitude. The frequencies of occurrence show (so far) no long-term trends. The seasonal cycles are not very clear but seem to reverse between more southern to more northern locations. Most profiles with ice-supersaturation have more than one supersaturated layer; this stacking increases as well to the north. Due to the 1‑Hz resolution of the data we find ice-supersaturated layers a few metres thick, but very thick layers extending over almost 5 km are found as well. Median thickness values are smaller than in previous studies, between 100 m and 200 m. The far northern locations display a strong seasonal cycle of the mean layer thickness with maxima in the polar night, probably caused by radiation cooling. Ice supersaturation occurs most frequently directly beneath the tropopause in an upper-tropospheric layer whose depth varies strongly seasonally, being thin in summer and much thicker in winter. Due to the very low temperatures in the Arctic ice supersaturation can occur at the ground. Temperatures in arctic supersaturated layers typically range from -40 to -60 °C, but can occasionally be lower than -70 °C. Water vapour volume mixing ratios range from a few to about 500 ppmv. The relative humidity with respect to ice can exceed 150-160 %. The thickness of supersaturated layers is weakly correlated with its maximum supersaturation, but not with temperature and absolute humidity.

Item URL in elib:https://elib.dlr.de/134905/
Document Type:Article
Title:On ice supersaturation over the Arctic
Authors:
AuthorsInstitution or Email of AuthorsAuthor's ORCID iD
Gierens, Klaus MartinDLR, IPAhttps://orcid.org/0000-0001-6983-5370
Wilhelm, LenaUniv. BonnUNSPECIFIED
Sommer, MichaelDWD, Meteorologisches Observatorium LindenbergUNSPECIFIED
Weaver, DanUniv. of Toronto Scarborough, Toronto, KanadaUNSPECIFIED
Date:2020
Journal or Publication Title:Meteorologische Zeitschrift
Refereed publication:Yes
Open Access:Yes
Gold Open Access:Yes
In SCOPUS:Yes
In ISI Web of Science:Yes
DOI :10.1127/metz/2020/1012
Page Range:pp. 1-12
Publisher:Borntraeger Science Publishers
ISSN:0941-2948
Status:Published
Keywords:ice supersaturation, Arctic, radiosonde data, GRUAN
HGF - Research field:Aeronautics, Space and Transport
HGF - Program:Space
HGF - Program Themes:Earth Observation
DLR - Research area:Raumfahrt
DLR - Program:R EO - Earth Observation
DLR - Research theme (Project):R - Atmospheric and climate research
Location: Oberpfaffenhofen
Institutes and Institutions:Institute of Atmospheric Physics
Institute of Atmospheric Physics > Earth System Modelling
Deposited By: Gierens, Dr.rer.nat. Klaus Martin
Deposited On:13 May 2020 12:33
Last Modified:13 May 2020 12:33

Repository Staff Only: item control page

Browse
Search
Help & Contact
Information
electronic library is running on EPrints 3.3.12
Copyright © 2008-2017 German Aerospace Center (DLR). All rights reserved.