HR: 1340h
AN: A23B-0786 [Abstracts]
TI: Simulation of observed changes in the North Atlantic Oscillation and surface climate in the latter half
of the 20th Century.
AU: * Scaife, A A
EM: adam.scaife@metoffice.gov.uk
AF: Hadley Centre,
Met Office, Fitzroy Road, Exeter, EX1 3PB
United Kingdom
AU: Knight, J R
EM: jeff.knight@metoffice.gov.uk
AF: Hadley Centre,
Met Office, Fitzroy Road, Exeter, EX1 3PB
United Kingdom
AU: Vallis, G K
EM: gkv@princeton.edu
AF: GFDL, Princeton University, Princeton, NJ NJ 08544
United States
AU: Folland, C K
EM: chris.folland@metoffice.gov.uk
AF: Hadley Centre,
Met Office, Fitzroy Road, Exeter, EX1 3PB
United Kingdom
AB:
The North Atlantic Oscillation (NAO) is the dominant pattern of winter variability in the climate of the Atlantic region.
The NAO also shows a large positive trend between the 1960s and 1990s which is manifested as a rapid increase in winter
surface temperature and rainfall in Northern Europe. Despite this, the cause of the trend remains a source of much debate
and it is not reproduced in simulations of the 20th century with global climate models. Constraining lower boundary
conditions using historical sea-surface temperature and sea-ice distributions allows models to reproduce a weak trend in the
NAO and land surface temperature. However, we find that the full observed trend can be reproduced when conditions in the
lower stratosphere are relaxed towards observations. This result indicates that upper level circulation changes and the
strength of the downward coupling to the surface are strong enough to explain a large fraction of the recent change in North
European and North American surface climate. It also suggests that upper level variability should be reproduced in models to
fully simulate surface climate variations, and that the response of the Atlantic region to anthropogenic forcing is strongly
influenced by natural variability on decadal timescales.
DE: 3362 Stratosphere/troposphere interactions
DE: 1610 Atmosphere (0315, 0325)
DE: 1620 Climate dynamics (3309)
SC: Atmospheric Sciences [A]
MN: 2004 AGU Fall Meeting