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SEMINAR: REMINDER - AOML Seminar - January 24, 2013 - 2:00 p.m. - AOML Library - Second floor - Professor Milton Halem - "Global Decadal Trends of Greenhouse Gases and Surface Temperature Linkages"
| From: | Aoml.Receptionist <aoml.receptionist@noaa.gov> |
| Subject: | SEMINAR: REMINDER - AOML Seminar - January 24, 2013 - 2:00 p.m. - AOML Library - Second floor - Professor Milton Halem - "Global Decadal Trends of Greenhouse Gases and Surface Temperature Linkages" |
| Date: | Wed, 23 Jan 2013 13:46:21 -0500 |
|
AOML
Seminar DATE: Thursday, January 24,
2013 1:45
p.m.) (Seating
is very limited) Gases
and Surface Temperature Linkages" AOML
Abstract. R. Goody et.
al., J. Harries et. al., and more recently others have shown
that changes in greenhouse gases can be detected in the spectrum
of outgoing long and short wave radiation
using climate model simulations as surrogates for observed
radiances. Ohring et. al., has shown that accuracies of 0.010K/yr
are adequate to resolve inter-annual changes in brightness temperatures.
In this talk, we present the first ever direct observations of
global decadal trends of greenhouse gases and their linkages to
surface temperatures. We compute the all-sky OLW spectrum for 2378 spectral infrared channels of the
AIRS instrument, launched in April, 2002, for every lat-lon grid
cell covering the Earth at 2.00x2.00 and
globally average these gridded radiances from all the AIRS footprints. Decadal
trends of increased GHGs are inferred from the AIRS spectra from
Jan. 1, 2003-Dec. 31, 2012 indicating continued decreases in the
trend of Surface Brightness Temperatures (BT) of CO2 (14.15u
and 4.3u), O3 BT (9.8u), CH4 BT (7.7u) and slightly positive
increases in the CFC11 and CFC12 BTs resp. of window channels at
8.7u and 11.1u, in accordance with results of the Montreal Protocol. No significant trends are seen in the global water cycle between 7.38u and 6.38u. We show the decadal stability of the AIRS instrument by comparisons with the MODIS IR spectral channels on the same satellite with views almost identical in space and time for 14 days in each September for 10 years. An annual BT warming trend of ~0.70K per decade is observed in the Arctic while global annual mean surface brightness temperature trends for the decade are essentially flat. An amplifying annual oscillation in surface BT is observed in the Antarctic with inter-annual increases growing from 0.10K to 0.40K over a decade which is speculated to be related to the MJO. AIRS surface BT has an annual correlation of 0.97with GISS Surface Temperatures (ST) and 0.82 with GISS monthly correlations, thus implying that surface BT can serve as a climate change proxy. Biographical
Sketch. Dr. Milton Halem is a Research Professor in the
Computer Science and Electrical Engineering Department at the
University of Maryland, Baltimore County since 2002. In
addition, he is Director, of the NSF sponsored Center for Hybrid
Multicore Productivity Research. His main teaching and research
areas of current interest are service oriented cloud computing, hybrid computational science, advanced information systems
and data intensive computing. Prior to joining UMBC, Dr. Halem
served from 1999 to 2002 as Assistant Director for Information
Sciences and Chief Information Officer at the NASA Goddard Space
Flight Center. From 1984 to 1999 he served as Chief of the Earth
and Space Data Computing Divison. He managed many of the most
powerful scientific data intensive supercomputing centers. He is nationally recognized
for his research in simulation studies of space observing
systems and four dimensional satellite data assimilation for
weather and climate prediction. He acquired his Bachelor's
degree in Mathematics from the City College of New York and a
Ph.D. in Mathematics from the Courant Institute of Mathematical
Sciences, New York University in 1968. In 1999, Dr. Halem received
an honorary Doctorate from Dalhousie University, CA in recognition
for his contributions to the field of computational science. Dr.
Halem is also a
noted fine art screenprinter. |
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