Title: ARC-IONS - First results from a North American Strategic Network
1- ARC-IONS - First results from a North American
Strategic Network - David W. Tarasick
- Experimental Studies, Air Quality Research
Division - A.M. Thompson (PSU), S.J. Oltmans (NOAA),
- G. Forbes (EC-MSC), J. Merrill (UNH)
- NASA Aura Validation (M.J. Kurylo K.W. Jucks)
ARCTAS (J. Crawford) - J. Davies, R. Mittermeier, W. Hocking, J. Witte
- G. Liu, C. Sioris, H. He, M.K. Osman, T.
Carey-Smith - L.B.J. McArthur, C. Banic K. Puckett (EC)
- The Green Horse Society, and most especially all
the many observers who obtained the ozonesonde
measurements at the ARC-IONS sites.
2Rationale
- Ozone soundings are the major source of
information on ozone amounts in the free
troposphere, capable of precise (3-5)
measurements of ozone with 100m vertical
resolution. While regular network soundings
(typically weekly) produce valuable data, such
soundings are often too sparse, both in space and
time, to answer some scientific questions. - Strategic networks are designed to answer
specific scientific questions, typically with
dense networks of daily launches that have
sufficient resolution in space and time to
resolve atmospheric dynamic variability. Launches
can be coordinated, often with collocated
aircraft or satellite measurements.
3ARC-IONS Sites
13 sites in Canada 5 in US 1 in Greenland
Largest ozonesonde intensive ever in Canada
4TES / ARCIONS comparison. Summary of stare
results for Bratts Lake, April 18th, 2008. Cloud
is optically thin. Sonde results show 5 - 10
bias at Barrow and 15 bias at Bratts Lake. 15
bias is consistent with lidar results.
5Walsingham windprofiler radar
6Double tropopause
An example of a double tropopause observed at
Churchill on April 18th, 2008. This event is due
to a large poleward intrusion of subtropical
tropospheric air and was forecast by the START08
project at NCAR (L. Pan, personal communication).
7Arctic Intensive Ozonesonde Network Study
(ARC-IONS) 2008
- Cooperation with NASA project Arctic Research of
the Composition of the Troposphere from Aircraft
and Satellites (ARCTAS), in April and July 2008
over northern Canada. - Objectives
- studies of boundary layer ozone depletions
resulting from halogens released from sea salt
deposited on Arctic sea ice - evaluation of the role of stratosphere/troposphere
exchange (STE) in the spring buildup of
tropospheric ozone - the contribution to the tropospheric ozone budget
from boreal forest fires and the extent of fire
emission influence on a trans-continental scale
and beyond - validation of Aura (TES, OMI) at high latitudes
of GEM-MACH, for ozone STE, and forest fire
models.
8Arctic Surface Ozone Depletions
- Arctic sites showed modest ozone depletion in the
surface boundary layer throughout the spring
campaign
9Arctic Surface Ozone Depletions
- This was occasionally severe.
10Tarasick and Bottenheim, ACP, 2, 197205, 2002.
11Sea ice? Temperature trends?
12Backtrajectories for the sonde launches of April
17th, 2008. These appear to correlate with the
large amounts of BrO observed by the OMI
instrument on April 16th, 2008. However, in other
examples this relationship is less clear.
13Do O3 depletions correlate with satellite BrO?
14Do O3 depletions correlate with satellite BrO?
15Do O3 depletions correlate with satellite BrO?
16Do O3 depletions correlate with satellite BrO?
17Ozone from the stratosphere?
M.K. Osman, UWO
18FLEXPART modeling seems to show good
correspondence with apparent intrusions
Intrusions associated with jumps in tropopause
height
T. Carey-Smith, NIWA
19TES Measurements Eureka
H. He, UWO/ARQX
20Radar tropopause height vs Brewer ozone
H. He, UWO/ARQX
21T. Carey-Smith NIWA
22Ozonesonde Climatology
Hysplit forward and back- trajectories applied to
ozone soundings fill in the NA map
23Ozonesonde Climatology
Correlations between OMI and trajectory-mapped
ozone soundings at different altitudes
- 3 hrs, Aug 2006
- 3 hrs, Mar-May, 2006
24Ozonesonde Climatology
25Ozonesonde Climatology
26- ARCTAS Data Workshop, January 27-30, Virginia
Beach - Spring AGU Meeting 24-27 May, 2009 (Toronto)
Session A10 Processes over Midlatitude North
America and the Arctic (2008) Observed from
Satellite and Field Campaigns Abstract
deadline 4 March 2009, 2359 UT. - MST12 (Radar) Workshop 17 - 23 May, 2009 London,
Ontario http//www.mst12.com/ Session
Tropopause processes and Stratospheric/Tropospheri
c Exchange Abstract deadline Friday January
23, 2009.
27Thank you!
28- Highlights of three IONS campaigns
- IONS-04 2004, mostly eastern North America 275
profiles, largest single set of free tropospheric
ozone measurements ever compiled (as of 2004) for
this region. Coordinated AQ model comparison,
aircraft surface measurements. - IONS-06 2006, three phases with 23 sites 740
profiles. Coordinated AQ model comparison,
aircraft surface measurements. Validation of
TES, OMI, MLS, ACE measurements coordination
with Aura ACE overpasses. - ARC-IONS (2008) Canada, Alaska and the lower
U.S.. Two phases with 18 sites, mostly daily
profiles. Coordination with NASA aircraft
flights. Validation of TES, OMI, MLS, ACE
measurements coordination with Aura ACE
overpasses. Coordination with special TES
Step-and-stare observations. - Also new tropospheric ozone lidars in operation
at Egbert (Toronto) and Eureka aerosol optical
depth (AOD) measurements from the Canadian
AERONet and Brewer networks, and an aerosol lidar
deployed near Yellowknife. Radar measurements of
tropopause height to detect stratospheric
intrusions, and to measure wave activity and
turbulence strengths associated with intrusion
events. Modeling studies using GEM-MACH,
GEM-FLEXPART and other systems, in order both to
validate the models and to interpret the data.
29H. He, UWO/ARQX
30M.K. Osman, UWO
31Ozonesonde Climatology
32IONS Publications (gt24 to date)
- Unique data sets provided by coordinated
intensive ozone profile measurements - tropospheric ozone processes contribution to
ozone budget model comparisons (Cooper et al.,
2006 2007 Thompson et al., 2007a,b Tarasick et
al., 2007 Pfister et al., 2008 Tang et al.,
2008) - pollution plumes from boreal forest fires (Morris
et al., 2006), New York City (Mao et al., 2006).
- stratospheric intrusions the tropopause
behaviour preceeding them (Hocking et al., 2007).
- validation of satellite measurements (Parrington
et al., 2007 Stajner et al., 2007 Schoeberl
et al., 2007 Nassar et al., 2007 Jiang et
al., 2007 Dupuy et al., 2007 Livingston et
al., 2007 Nardi et al., 2007) and of models
(Chai et al., 2007 Pierce et al., 2007 Yu et
al., 2007).
33Sea ice? Temperature trends?
34Ozonesonde Climatology
35EC Regional AQ models AURAMS CHRONOS compared
with IONS-04 sonde data
- forecast errors 25-75
- low bias in upper troposphere
- GEM-MACH global, full stratosphere
36Comparison of GEOS-Chem with Ozonesonde Data
Wallops (76W, 38N) 19 July 2005
Churchill (95W, 58N) 20 July 2005
Assimilation improves the O3 distribution in the
UTLS region
Pressure (hPa)
Pressure (hPa)
Ozone (ppb)
Ozone (ppb)
Wallops (76W, 38N) 26 July 2005
Eureka (85W, 80N) 20 July 2005
O3 plume is redistributed throughout column in
assimilation
Pressure (hPa)
Pressure (hPa)
Ozone (ppb)
Ozone (ppb)
37Stratosphere-Troposphere Exchange
AM2-Chem ozone (120W 2100 GMT, July 26)
AM2-Chem ozone analysis
GEOS-Chem ozone (120W 2100 GMT, July 26)
GEOS-Chem ozone analysis
Stratospheric intrusion at 40ºN more pronounced
in both models following assimilation
38Tropospheric Ozone DIAL - First ResultsARC-IONS
Campaign
Generated a DIAL ozone profile for full day and 2
hours centred at ozonesonde launch time Generally
not much difference between full and coincident
profiles DIAL shows similar features to
ozonesonde profile, does not show an increase in
ozone concentration with altitude
39H. He, UWO/ARQX