○AGU●
☆GRL☆
1. Tide-induced microseismicity in the Mertz
glacier grounding area, East Antarctica
Guilhem Barruol, Emmanuel
Cordier, Jérôme Bascou, Fabrice R. Fontaine, Benoit Legrésy and Lydie
Lescarmontier
Accepted
manuscript online: 7 OCT 2013 10:43AM EST | DOI: 10.1002/2013GL057814
2. Uncertainties in future ozone and PM10 projections over
Europe from a regional climate multi-physics ensemble
P. Jiménez-Guerrero, S. Jerez, J. P.
Montávez and R. M. Trigo
Accepted
manuscript online: 9 OCT 2013 03:50AM EST | DOI: 10.1002/2013GL057403
3. Sea-surface
temperature and sea-ice variability in the sub-polar North Atlantic from
explosive volcanism of the Late 13th century
M.-A. Sicre, M. Khodri, J. Mignot, J. Eiriksson,
K.-L. Knudsen, U. Ezat, I. Closset, P. Nogues and G. Massé
Accepted
manuscript online: 10 OCT 2013 09:07AM EST | DOI: 10.1002/2013GL057282
4. Biophysical
Responses near Equatorial Islands in the Western Pacific Ocean during El
Niño/La Niña Transitions
Michelle M. Gierach, Monique Messié, Tong
Lee, Kristopher B. Karnauskas and Marie-Hélène Radenac
Accepted
manuscript online: 11 OCT 2013 01:45AM EST | DOI: 10.1002/2013GL057828
Key Points
Chl-a blooms near
the Gilbert Islands during some El Nino/La Nina transitions
Distinct physical
conditions are necessary for blooms to occur in this region
Ocean
preconditioning from El Nino and wind forcing from La Nina control blooms
5. Oceanic
Control of Sea Level Rise Patterns along the East Coast of the United States
Jianjun Yin and Paul B. Goddard
Accepted
manuscript online: 11 OCT 2013 09:05PM EST | DOI: 10.1002/2013GL057992
6. NAO
implicated as a predictor of Northern Hemisphere mean temperature multidecadal
variability
Jianping Li, Cheng Sun and Fei-Fei Jin
Accepted
manuscript online: 11 OCT 2013 10:38PM EST | DOI: 10.1002/2013GL057877
Key Points
The NAO leads the
DNHT by 15-20 years in the observations.
The slow oceanic
processes may account for the time lead of NAO leading DNHT.
A NAO-based model
is a useful predictive tool for the NHT.
☆Paleoceanography☆
1. Near-collapse
of the meridional SST gradient in the Eastern Equatorial Pacific during the
Heinrich Stadial 1
Stephanie S Kienast, Tobias Friedrich,
Nathalie Dubois, Paul S Hill, Axel Timmermann and Markus Kienast
Accepted
manuscript online: 7 OCT 2013 11:06AM EST | DOI: 10.1002/2013PA002499
Key Points
SSTs and dust
input are reconstructed for the last 25 ka in the EEP
A freshwater
hosing experiment is carried out with a coupled climate model
Meridional SST
gradient minimal and dust input maximal during Heinrich Stadial
☆G3☆
☆GBC☆
☆JGR Oceans☆
特になし
○EGU●
1. Why could
ice ages be unpredictable?
M. Crucifix
doi:10.5194/cp-9-2253-2013
2. Inferred
changes in El Niño–Southern Oscillation variance over the past six centuries
S. McGregor,
A. Timmermann, M. H. England, O. Elison Timm, and
A. T. Wittenberg
doi:10.5194/cp-9-2269-2013
3. Mid- and
late Holocene dust deposition in western Europe: the Misten peat bog (Hautes
Fagnes – Belgium)
M. Allan,
G. Le Roux, N. Piotrowska, J. Beghin, E. Javaux,
M. Court-Picon, N. Mattielli, S. Verheyden, and N. Fagel
doi:10.5194/cp-9-2285-2013
