Premium
Anomalous winter hydroxyl temperatures at 69°S during 2002 in a multiyear context
Author(s) -
French W. John R.,
Burns Gary B.,
Espy Patrick J.
Publication year - 2005
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2004gl022287
Subject(s) - anomaly (physics) , atmospheric sciences , climatology , context (archaeology) , environmental science , stratosphere , amplitude , mesosphere , airglow , geology , physics , paleontology , condensed matter physics , quantum mechanics
Hydroxyl airglow temperatures measured over Davis station, Antarctica (68°S, 78°E) in 2002 are compared to an 8‐year climatological mean. The 2002 winter average temperature was 5.1 ± 0.8K warmer than the climatological mean. This anomaly is a factor of two larger than what can be attributed to solar flux increases. Of the 210 nightly averages obtained, 72 (34%) exceeded the climatological maximum, primarily in two unusually warm intervals in late‐May to early‐June and in mid‐July. An unusually cold interval (10 nights below the climatological minimum) coincided with a climatological dip in mid‐August. Temperature oscillations of 15–20 K amplitude, extending over 4 cycles across the Sep–Oct stratospheric warming correlate with Rothera temperatures and Davis mesospheric winds and are consistent with a 14‐day westward propagating zonal planetary wave number 1.
Accelerating Research
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom
Address
John Eccles HouseRobert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom