Start Date/Time: Thursday, May 05, 2011, 3:30 PM
Location: JHN 102
Anais Orsi, a senior graduate student with Jeff Severinghaus at Scripps,
will be giving the ESS colloquium on Thursday, May 5th at 3:30 in
Johnson 102.
Anais will speak about her innovative work combining 15N of gas in ice
cores with borehole thermometry to obtain a state-of-the art
paleotemperature history in Antarctica.
Anais will be around much of the week, and you can contact Eric Steig
(steig@uw) if you would be interested in meeting with her.
Abstract:
We present a record of temperature and accumulation at WAIS Divide for
the last 1000 years using noble gas isotopes.
The isotopes of nitrogen, argon and krypton in air bubbles reflect
changes in the firn thickness as well as temperature gradients between
the surface and the depth at which bubbles close. We used krypton and
argon isotopes in WDC05A to estimate changes in the firn thickness,
which is sensitive to both temperature and accumulation. The results are
consistent with estimates of the accumulation rate obtained from layer
counting, and they provide a useful constraint on firn densification
models. d15N from WDC06A was then corrected and integrated to produce an
estimate of surface temperature over time. In addition, observed
borehole temperature from the 300m WDC05A hole provides an independent
long term surface temperature record. Both methods agree well, and
provide a test of the validity of d18Oice as a thermometer. The results
show that West Antarctic centennial mean temperature was cooling from
1000 to 1765 (+-20) CE , and has been on a long term warming trend
since. There is significant multi-decadal variability in temperature,
with an amplitude of at least 0.5C. The recent warming trend of
0.29C/decade since 1958, established by Steig et al (2009) is confirmed
by this work, and placed in the broader context of the last millennium.