HR: 17:20h
AN: U24D-05 [Abstracts]
TI: Arctic transport climatologies for the International Arctic System for Observing the Atmosphere
(IASOA) and POLARCAT
AU: * John, B F
EM: jfb@nilu.no
AF: Department of Atmospheric and Climate Research, Norwegian Institute for Air Research
(NILU), P.O. Box 100, Kjeller, NO 2027, Norway
AU: * John, B F
EM: jfb@nilu.no
AF: School of Engineering, University of California, Merced, P.O. Box 2039, Merced, CA 95304,
United States
AU: Stohl, A
EM: ast@nilu.no
AF: Department of Atmospheric and Climate Research, Norwegian Institute for Air Research
(NILU), P.O. Box 100, Kjeller, NO 2027, Norway
AU: Eckhardt, S
EM: sec@nilu.no
AF: Department of Atmospheric and Climate Research, Norwegian Institute for Air Research
(NILU), P.O. Box 100, Kjeller, NO 2027, Norway
AU: Uttal, T
EM: Taneil.Uttal@noaa.gov
AF: National Oceanic and Atmospheric Administration/Earth System Research Laboratory,
David Skaggs Research Building, Broadway, Boulder, CO 80305, United States
AU: Ocko, I
EM: ilocko@umich.edu
AF: Atmospheric, Ocean and Space Sciences, University of Michigan, 2455 Hayward St., Ann Arbor, MI 48109, United States
AU: Tørseth, K
EM: kt@nilu.no
AF: Department of Atmospheric and Climate Research, Norwegian Institute for Air Research
(NILU), P.O. Box 100, Kjeller, NO 2027, Norway
AB:
Several intensive campaigns have recently focused on the transformation and transport of pollutants to the Arctic.
During the International Polar Year large-scale coordinated aircraft campaigns will be conducted throughout the
circum-Arctic as a part of the POLARCAT project. Additionally, measurements at surface based sites in the IASOA
network will be coordinated to capture unique transport events. Toward improved interpretation of the
measurements, 10-year transport climatologies are being developed using the Lagrangian particle dispersion
model FLEXPART.
This paper presents the climatologies for IASOA network, but also introduces FLEXPART products available for
the aircraft campaigns. Climatologies are based on 20-day backward model runs for each station using globally
gridded 1°x1° input fields from the European Center for Medium Range Weather Forecasting (ECMWF). For
analysis of specific measurements, model output for each station is generated at six hour intervals (0, 6, 12, 18
UTC). There are 60 vertical levels, switching to 92 after March, 2006 in the input data. Calculations are based on
the release of 40,000 particles representing an idealized inert tracer with an infinite lifetime allowing for
interpretation of the results by a wide range of experimentalists. The generated source-receptor relationships are
averaged into a seasonal climatology for the various locations.
We present ‘retroplumes' or three-dimensional Potential Emissions Sensitivity (PES) for the stations. The PES (s
kg-1) in each grid cell is proportional to the particle residence time in the cell. For a given source with unit
strength (1 kg s-1) the PES provides the simulated mixing ratio at the receptor site. A cluster analysis of
particle locations also provides the ability to evaluate the proportion of particles residing in the stratosphere. From
this analysis we provide, in addition to the PES, the cluster centroid locations, most analogous to traditional
trajectories. Initial results from a concurrent study with HYSPLIT showing seasonal trajectories are also
presented
UR: http://transport.nilu.no
DE: 0368 Troposphere: constituent transport and chemistry
DE: 1610 Atmosphere (0315, 0325)
DE: 1616 Climate variability (1635, 3305, 3309, 4215, 4513)
DE: 3305 Climate change and variability (1616, 1635, 3309, 4215, 4513)
DE: 9315 Arctic region (0718, 4207)
SC: Union [U]
MN: 2007 Fall Meeting