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Click to see the full-text of: Article: Drought variability at the northern fringe of the Asian summer monsoon region over the past millennia. Clim Dyn. 1 3 DOI 10.1007/s00382-015-2839-z Clim Dyn (2015) 45:2963 ERRATUM Erratum to: Influence of ocean–atmospheric oscillations on lake ice phenology in eastern North America. Official Full-Text Publication: An Atlantic influence on Amazon rainfall. Clim Dyn on ResearchGate, the professional network for scientists.

By Clim Dyn, Julien Cattiaux, Herve Douville, Aurelien Ribes, Fabrice Chauvin, Chloe Plante, J. Cattiaux and C. Plante. Usage ecospat.grid.clim.dyn (glob, glob1, sp, R, th.sp, th.env) Arguments glob A two-column dataframe (or a vector) of the environmental values (in column) for. Clim Dyn DOI 10.1007/s00382-011-1092-3 Why does the Antarctic Peninsula Warm in climate simulations? (2010).

Drought variability at the northern fringe of the Asian summer monsoon

Mareschal and Beltrami: Evidence for recent warming in eastern This yields an underdetermined system of linear equa- tions which can be solved for Tk by. Clim Dyn manuscript No. The potential to narrow uncertainty in projections of regional precipitation change (2010). Lheveder Li Sevault Somot Aout2013 Clim Dyn. Uploaded by. B. Peneau L.Heveder. Interannual variability of deep convection in the Northwestern Mediterranean.

Erratum to: Influence of ocean–atmospheric oscillations on lake ice.

Clim Dyn manuscript No. The potential to narrow uncertainty in projections of regional precipitation change (2010). Lheveder Li Sevault Somot Aout2013 Clim Dyn. Uploaded by. B. Peneau L.Heveder. Interannual variability of deep convection in the Northwestern Mediterranean. Clim Dyn 28:743–758 Murtugudde R, McCreary J, Busalcchi A (2000) Oceanic processes associated with anomalous events in the Indian Ocean. J Geophys Res. Author version: Clim. Dyn., vol.41. 2013. 381-402 Decadal and long-term sea level variability in the tropical Indo-Pacific Ocean A G Nidheesh1, Matthieu Lengaigne 2,1. Dr. George Boer Canadian Centre for Climate Modelling and Analysis. Accepted for publication in Clim. Dyn. doi 10.1007/s00382-012-1600-0. Yu, B. F.W. Zwiers. Clim Dyn, in press (published online 26 February 2008). Mao J, Chan JCL, Wu G (2004) Relationship between the onset of the south China sea summer.

Lheveder Li Sevault Somot Aout2013 Clim Dyn - Academia.edu

1 Author version: Clim. Dyn., vol.38. 2012. 1521-1543 TropFlux: Air-Sea Fluxes for the Global Tropical Oceans – Description and evaluation against observations. 1 3 DOI 10.1007/s00382-014-2300-8 Clim Dyn (2015) 45:47–65 Optimal forcing of ENSO either side of the 1970’s climate shift and its implications for predictability. Clim Dyn DOI 10.1007/s00382-013-1884-8 Author.s personal copy. their signi?cance, the representation of clouds in global climate and weather models has been.

Clim Dyn manuscript No. The potential to narrow uncertainty in.

Clim Dyn DOI 10.1007/s00382-013-1884-8 Author.s personal copy. their signi?cance, the representation of clouds in global climate and weather models has been. Clim Dyn How sensitive are the Pacific–tropical North Atlantic teleconnections to the position and intensity of El Nino?related warming. Clim. Dyn., in press Cai, W., A. Santoso, G. Wang, S-W Yeh, S.-I. Earlier publications: Marti O., P. Braconnot, J.-L. Dufresne, J. Bellier. Cloud vertical distribution from radiosonde, remote sensing, and model simulations Jinqiang Zhang Zhanqing Li Hongbin Chen Hyelim Yoo Maureen Cribb. Personal homepage. Ivan Guttler. following the weather since 1985. Contents. 1 Contact. 2 Interest. 3 Publications. 4 Projects. Clim. Dyn., 41, 2555–2575. Clim Dyn (2007) 28:797–811 DOI 10.1007/s00382-006-0212-y. of the Yangtze River, Japan, and Changma over Korea, and rainfall over northern China (Dao and Chen 1957.

Reduction of the thermocline feedback associated with mean SST bias in ENSO simulation. Clim Dyn (2012) 39:1413–1430 DOI 10.1007/s00382-011-1164-4. Clim Dyn (2007) 29:293–303 DOI 10.1007/s00382-007-0236-y. East Asian summer monsoon rainfall moves to northern China. Moreover, the subtropical high over the western. Clim Dyn (2008) 30:145–160 DOI 10.1007/s00382-007-0278-1. depths to the water table but highly variable surface soil wetness (Hinzman et al. 1991).

How sensitive are the Pacific–tropical North Atlantic teleconnections.