Investigating physical and chemical changes in atmospheric circulation, ozone depletion, temperatures and sea-ice extent in both Polar Regions can help determine how much of the observed change is due to human activity and how much is a result of natural factors. Unique chemical processes occur in the atmosphere above Antarctica and the Arctic reveal much about our changing world.

Understanding the atmosphere and the ozone layer – a short film from UNEP

 

 

ISOL-ICE

PI: Markus M. Frey Co-I’s: X. Yang, R. Mulvaney NERC Grant: NE/N011813/1 The ozone layer shields all land-based life forms from harmful ultraviolet radiation; and indirectly influences the climate at …


Filchner Ice Shelf System, Antarctica

Understanding the contribution that polar ice sheets make to global sea-level rise is recognised internationally as urgent.  The mission of this five-year project is to capture new observations and data …


DRIIVE

DRIIVE will use the new EISCAT_3D radar to understand multi-scale coupling in the Ionopshere and how it is influenced both by space weather and the lower atmosphere.  The impact of …


SWIMMR-T

Space debris is emerging as a key problem for humanity with the potential to cause major socio-economic impacts. It is currently estimated that there are over 900,000 pieces of debris …



A recent pause in Antarctic Peninsula warming

20 July, 2016

The rapid warming of the Antarctic Peninsula, which occurred from the early-1950s to the late 1990s, has paused. Stabilisation of the ozone hole along with natural climate variability were significant in bringing about the change. Together these influences have now caused the northern part of the peninsula to enter a temporary cooling phase. Temperatures remain higher than measured during the middle of the 20th Century and glacial retreat is still taking place. However, scientists predict that if greenhouse gas concentrations continue to rise at the current rate, temperatures will increase across the Antarctic Peninsula by several degrees Centigrade by the end of this century.


Ocean warming primary cause of glacier retreat

14 July, 2016

A new study has found for the first time that ocean warming is the primary cause of retreat of glaciers on the Antarctic Peninsula. The Peninsula is one of the largest current contributors to sea-level rise and this new finding will enable researchers to make better predictions of ice loss from this region.



Carbon dioxide level breached at Halley VI

16 June, 2016

Levels of the greenhouse gas carbon dioxide (CO2) in the atmosphere – which is the leading driver of recent climate change – have reached a milestone at British Antarctic Survey’s …



FEATURED PAPER: Polar Vortex teleconnection

26 January, 2016

This paper provides new evidence and proposes a new dynamical mechanism for the teleconnection between the two largest jet streams in the northern winter stratosphere – the tropical wind system …


FEATURED PAPER: Improving air quality models

13 October, 2015

Recent research in polar and non-polar regions showed that sun-lit snow packs are important chemical reactors and reservoirs, which strongly influence air quality of the lower atmosphere and likely also …