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@ARTICLE{Gaudel:845669,
author = {Gaudel, A. and Cooper, O. R. and Ancellet, G. and Barret,
B. and Boynard, A. and Burrows, J. P. and Clerbaux, C. and
Coheur, P. -F. and Cuesta, J. and Cuevas, E. and Doniki, S.
and Dufour, G. and Ebojie, F. and Foret, G. and Garcia, O.
and Granados Muños, M. J. and Hannigan, J. W. and Hase, F.
and Huang, G. and Hassler, B. and Hurtmans, D. and Jaffe, D.
and Jones, N. and Kalabokas, P. and Kerridge, B. and
Kulawik, S. S. and Latter, B. and Leblanc, T. and Le
Flochmoën, E. and Lin, W. and Liu, J. and Liu, X. and
Mahieu, E. and McClure-Begley, A. and Neu, J. L. and Osman,
M. and Palm, M. and Petetin, H. and Petropavlovskikh, I. and
Querel, R. and Rahpoe, N. and Rozanov, A. and Schultz,
Martin and Schwab, J. and Siddans, R. and Smale, D. and
Steinbacher, M. and Tanimoto, H. and Tarasick, D. W. and
Thouret, V. and Thompson, A. M. and Trickl, T. and
Weatherhead, E. and Wespes, C. and Worden, H. M. and
Vigouroux, C. and Xu, X. and Zeng, G. and Ziemke, J.},
title = {{T}ropospheric {O}zone {A}ssessment {R}eport: {P}resent-day
distribution and trends of tropospheric ozone relevant to
climate and global atmospheric chemistry model evaluation},
journal = {Elementa},
volume = {6},
number = {1},
issn = {2325-1026},
address = {Washington, DC},
publisher = {BioOne},
reportid = {FZJ-2018-02881},
pages = {39 -},
year = {2018},
abstract = {The Tropospheric Ozone Assessment Report (TOAR) is an
activity of the International Global Atmospheric Chemistry
Project. This paper is a component of the report, focusing
on the present-day distribution and trends of tropospheric
ozone relevant to climate and global atmospheric chemistry
model evaluation. Utilizing the TOAR surface ozone database,
several figures present the global distribution and trends
of daytime average ozone at 2702 non-urban monitoring sites,
highlighting the regions and seasons of the world with the
greatest ozone levels. Similarly, ozonesonde and commercial
aircraft observations reveal ozone’s distribution
throughout the depth of the free troposphere. Long-term
surface observations are limited in their global spatial
coverage, but data from remote locations indicate that ozone
in the 21st century is greater than during the 1970s and
1980s. While some remote sites and many sites in the heavily
polluted regions of East Asia show ozone increases since
2000, many others show decreases and there is no clear
global pattern for surface ozone changes since 2000. Two new
satellite products provide detailed views of ozone in the
lower troposphere across East Asia and Europe, revealing the
full spatial extent of the spring and summer ozone
enhancements across eastern China that cannot be assessed
from limited surface observations. Sufficient data are now
available (ozonesondes, satellite, aircraft) across the
tropics from South America eastwards to the western Pacific
Ocean, to indicate a likely tropospheric column ozone
increase since the 1990s. The 2014–2016 mean tropospheric
ozone burden (TOB) between 60˚N–60˚S from five satellite
products is 300 Tg ± $4\%.$ While this agreement is
excellent, the products differ in their quantification of
TOB trends and further work is required to reconcile the
differences. Satellites can now estimate ozone’s global
long-wave radiative effect, but evaluation is difficult due
to limited in situ observations where the radiative effect
is greatest.},
cin = {IEK-8 / JSC},
ddc = {550},
cid = {I:(DE-Juel1)IEK-8-20101013 / I:(DE-Juel1)JSC-20090406},
pnm = {243 - Tropospheric trace substances and their
transformation processes (POF3-243) / 512 - Data-Intensive
Science and Federated Computing (POF3-512) / Earth System
Data Exploration (ESDE)},
pid = {G:(DE-HGF)POF3-243 / G:(DE-HGF)POF3-512 /
G:(DE-Juel-1)ESDE},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000431754000001},
doi = {10.1525/elementa.291},
url = {https://juser.fz-juelich.de/record/845669},
}