Zobrazeno 1 - 10
of 81
pro vyhledávání: '"D. P. Stevens"'
Publikováno v:
Earth System Dynamics, Vol 14, Pp 443-455 (2023)
The 18.6-year lunar nodal cycle arises from variations in the angle of the Moon's orbital plane. Previous work has linked the nodal cycle to climate but has been limited by either the length of observations analysed or geographical regions considered
Externí odkaz:
https://doaj.org/article/c81750f66d9e463599302103918dbfe3
Publikováno v:
The Cryosphere, Vol 16, Pp 3005-3019 (2022)
Floating ice shelves buttress the Antarctic Ice Sheet, which is losing mass rapidly mainly due to ocean-driven melting and the associated disruption to glacial dynamics. The local ocean circulation near ice shelves is therefore important for the pred
Externí odkaz:
https://doaj.org/article/6f0c8d7148ef45998665ecea825af577
Publikováno v:
Ocean Science, Vol 18, Pp 839-855 (2022)
CMIP6 model sea surface temperature (SST) seasonal extrema averaged over 1981–2010 are assessed against the World Ocean Atlas (WOA18) observational climatology. We propose a mask to identify and exclude regions of large differences between three co
Externí odkaz:
https://doaj.org/article/ac649e73341b4888adb453bcc233f24a
Publikováno v:
Geoscientific Model Development, Vol 14, Pp 275-293 (2021)
FORTE 2.0 is an intermediate-resolution coupled atmosphere–ocean general circulation model (AOGCM) consisting of the Intermediate General Circulation Model 4 (IGCM4), a T42 spectral atmosphere with 35σ layers, coupled to Modular Ocean Model – Ar
Externí odkaz:
https://doaj.org/article/895a684474f24cb3b2cf300637edf522
Publikováno v:
Geoscientific Model Development, Vol 8, Iss 10, Pp 3119-3130 (2015)
Most CMIP5 (Coupled Model Intercomparison Project Phase 5) models unrealistically form Antarctic Bottom Water by open ocean deep convection in the Weddell and Ross seas. To identify the mechanisms triggering Southern Ocean deep convection in models,
Externí odkaz:
https://doaj.org/article/8efbc2c333c1453fb7bebef9f1a0dcca
Autor:
I. G. Stevens, D. P. Stevens
Publikováno v:
Annales Geophysicae, Vol 17, Pp 971-982 (1999)
Passive tracers are used in an off-line version of the United Kingdom Fine Resolution Antarctic Model (FRAM) to highlight features of the circulation and provide information on the inter-ocean exchange of water masses. The use of passive tracers a
Externí odkaz:
https://doaj.org/article/e0389317b18740ae93ea33988a25daac
Autor:
M. I. Beare, D. P. Stevens
Publikováno v:
Annales Geophysicae, Vol 15, Pp 1369-1377 (1997)
This paper presents the development of a general-purpose parallel ocean circulation model, for use on a wide range of computer platforms, from traditional scalar machines to workstation clusters and massively parallel processors. Parallelism is pr
Externí odkaz:
https://doaj.org/article/518c5120659e4adfa0121a5da86d7933
Autor:
D. P. Stevens, S. R. Thompson
Publikováno v:
Annales Geophysicae, Vol 12, Pp 826-839 (1994)
The geographical area covered by the Fine-Resolution Antarctic Model (FRAM) includes that part of the South Atlantic south of 24°S. A description of the dynamics and thermodynamics of this region of the model is presented. Both the mean and eddy
Externí odkaz:
https://doaj.org/article/e8a515abb74a49c9ac890891003b8094
Autor:
D. P. Stevens, S. R. Thompson
Publikováno v:
Annales Geophysicae, Vol 12, Iss 9, Pp 826-839 (0000)
The geographical area covered by the Fine-Resolution Antarctic Model (FRAM) includes that part of the South Atlantic south of 24°S. A description of the dynamics and thermodynamics of this region of the model is presented. Both the mean and eddy fie
Externí odkaz:
https://doaj.org/article/38ff8fae47a44972a3bc446ded6a5014
