Zobrazeno 1 - 10
of 83
pro vyhledávání: '"M. Erpicum"'
Publikováno v:
The Cryosphere, Vol 9, Iss 3, Pp 945-956 (2015)
We have performed a future projection of the climate and surface mass balance (SMB) of Svalbard with the MAR (Modèle Atmosphérique Régional) regional climate model forced by MIROC5 (Model for Interdisciplinary Research on Climate), following the R
Externí odkaz:
https://doaj.org/article/c7ee9f72617142639da3b54f15c3840f
Publikováno v:
The Cryosphere, Vol 9, Iss 1, Pp 83-101 (2015)
With the help of the regional climate model MAR (Modèle Atmosphérique Régional) forced by the ERA-Interim reanalysis (MARERA) and the MIROC5 (Model for Interdisciplinary Research on Climate) global model (MARMIROC5) from the CMIP5 (Coupled Model
Externí odkaz:
https://doaj.org/article/7644e77f92064883ac56ba3849fee3b0
Publikováno v:
The Cryosphere, Vol 9, Iss 1, Pp 53-64 (2015)
A significant increase in the summertime occurrence of a high pressure area over the Beaufort Sea, the Canadian Arctic Archipelago, and Greenland has been observed since the beginning of the 2000s, and particularly between 2007 and 2012. These circul
Externí odkaz:
https://doaj.org/article/c563b37367f7456280a08f534c427d6a
Publikováno v:
The Cryosphere, Vol 8, Iss 5, Pp 1871-1883 (2014)
During recent summers (2007–2012), several surface melt records were broken over the Greenland Ice Sheet (GrIS). The extreme summer melt resulted in part from a persistent negative phase of the North Atlantic Oscillation (NAO), favoring warmer atmo
Externí odkaz:
https://doaj.org/article/24cbd09e9db74487be01372f4eb9137c
Publikováno v:
The Cryosphere, Vol 7, Iss 1, Pp 241-248 (2013)
Since 2007, there has been a series of surface melt records over the Greenland ice sheet (GrIS), continuing the trend towards increased melt observed since the end of the 1990's. The last two decades are characterized by an increase of negative phase
Externí odkaz:
https://doaj.org/article/c71e2a5ebc8c4778b132b274b65c105f
Publikováno v:
The Cryosphere, Vol 7, Iss 1, Pp 1-18 (2013)
In this study, simulations at 25 km resolution are performed over the Greenland ice sheet (GrIS) throughout the 20th and 21st centuries, using the regional climate model MAR forced by four RCP scenarios from three CMIP5 global circulation models (GCM
Externí odkaz:
https://doaj.org/article/3653492403b241dab709df0df7efaa0f
Publikováno v:
The Cryosphere, Vol 6, Iss 3, Pp 695-711 (2012)
With the aim to force an ice dynamical model, the Greenland ice sheet (GrIS) surface mass balance (SMB) was modelled at different spatial resolutions (15–50 km) for the period 1990–2010, using the regional climate model MAR (Modèle Atmosphériqu
Externí odkaz:
https://doaj.org/article/94b6aa51e0e04dbfacf66b1190dbfcd2
Publikováno v:
Nonlinear Processes in Geophysics, Vol 17, Iss 3, Pp 269-272 (2010)
Recently, new cycles, associated with periods of 30 and 43 months, respectively, have been observed by the authors in surface air temperature time series, using a wavelet-based methodology. Although many evidences attest the validity of this method a
Externí odkaz:
https://doaj.org/article/c2abc291dfc64402be042926e367ac58
Publikováno v:
The Cryosphere, Vol 2, Iss 2, Pp 117-129 (2008)
Results from a regional climate simulation (1970–2006) over the Greenland ice sheet (GrIS) reveals that more than 97% of the interannual variability of the modelled Surface Mass Balance (SMB) can be explained by the GrIS summer temperature anomaly
Externí odkaz:
https://doaj.org/article/6661b517c5be4c789faf75faefa89899
Publikováno v:
Nonlinear Processes in Geophysics, Vol 17, Iss 3, Pp 269-272 (2010)
Recently, new cycles, associated with periods of 30 and 43 months, respectively, have been observed by the authors in surface air temperature time series, using a wavelet-based methodology. Although many evidences attest the validity of this method a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::cfe33f7ffe95e5cdfda2a22c9c26e296
https://www.nonlin-processes-geophys.net/17/269/2010/
https://www.nonlin-processes-geophys.net/17/269/2010/
