Skip to content
Research Article Open access CC BY 4.0

Signs of Stability of the Arctic Sea Ice Thickness from Cryosat-2

A. Parker

Physical Science International Journal · pp. 1–8 · Published 22 Dec 2015

10.9734/PSIJ/2016/22017

Abstract

The signs of stability of the sea ice thickness from the latest Cryosat-2 results for the Arctic sea ice thickness are consistent with the Lower Troposphere Temperatures (LTT) and the sea ice extension results available since 1979. In the longer term, the current Arctic climate is probably at the start a cooling and recovery phase part of the same quasi-60 years’ oscillation that was responsible of most of the warming since the late 1970s. This natural variability is superimposed on a longer-term trend of warming temperatures and shrinking of sea ice that started in the 1800s.  

Arctic sea ice temperature climate models simulations experiments

Cited by 0

No indexed citations yet.

Article metrics

Real usage data collected on this platform.

0

Page views

0

PDF downloads

0

Outbound clicks

0

Citations

Views by country

Approximate, from request IP at view time — not citizenship or institution. Countries with fewer than 5 views are grouped as "Other".

No views recorded yet.

Traffic sources

Referring site, by host.

No traffic recorded yet.

Views and downloads exclude known bots/crawlers. Citations combines this platform's own DOI-resolved index with each external source's own reported total — see Cited by above for individually listed citing works. Last refreshed 0 seconds ago.