Open Access
Open access
volume 14 pages 127-130

Antarctic and Southern Ocean Sea-Ice and Climate Trends

Jacka T.H.
Publication typeJournal Article
Publication date1990-01-01
scimago Q2
wos Q3
SJR0.668
CiteScore3.4
Impact factor2.1
ISSN02603055, 17275644
Earth-Surface Processes
Abstract

A computer-based climate monitoring project is described. Data sets include monthly and annual mean surface temperatures and pressures for occupied stations in Antarctica, the Southern Ocean and South Pacific Ocean; and monthly Antarctic sea-ice extent at each 10° of longitude.

Simple statistical analyses of the data sets reveal a mean warming of ~0.15°C (10 a)−1 since the mid 1950s for Antarctic coastal stations and of ~0.04°C (10 a)−1 since the mid 1940s for the ocean stations. The sea-ice record from 1973 to 1988 reveals that the average northern ice limit has decreased at ~0.23°lat. (10 a)−1. Despite apparently compatible long-term trends of temperature and sea-ice extent, annual fluctuations of temperature and ice extent are highly variable and are not well correlated.

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GOST Copy
Jacka T. H. Antarctic and Southern Ocean Sea-Ice and Climate Trends // Annals of Glaciology. 1990. Vol. 14. pp. 127-130.
GOST all authors (up to 50) Copy
Jacka T. H. Antarctic and Southern Ocean Sea-Ice and Climate Trends // Annals of Glaciology. 1990. Vol. 14. pp. 127-130.
RIS |
Cite this
RIS Copy
TY - JOUR
DO - 10.1017/S0260305500008417
UR - https://doi.org/10.1017/S0260305500008417
TI - Antarctic and Southern Ocean Sea-Ice and Climate Trends
T2 - Annals of Glaciology
AU - Jacka, T H
PY - 1990
DA - 1990/01/01
PB - Cambridge University Press
SP - 127-130
VL - 14
SN - 0260-3055
SN - 1727-5644
ER -
BibTex
Cite this
BibTex (up to 50 authors) Copy
@article{1990_Jacka,
author = {T H Jacka},
title = {Antarctic and Southern Ocean Sea-Ice and Climate Trends},
journal = {Annals of Glaciology},
year = {1990},
volume = {14},
publisher = {Cambridge University Press},
month = {jan},
url = {https://doi.org/10.1017/S0260305500008417},
pages = {127--130},
doi = {10.1017/S0260305500008417}
}