An evaluation of the E3SMv1 Arctic ocean and sea-ice regionally refined model
نویسندگان
چکیده
Abstract. The Energy Exascale Earth System Model (E3SM) is a state-of-the-science system model (ESM) with the ability to focus horizontal resolution of its multiple components in specific areas. Regionally refined global ESMs are motivated by need explicitly resolve, rather than parameterize, relevant physics within regions resolution, while offering significant computational cost savings relative respective configurations high-resolution (HR) everywhere on globe. In this paper, we document results from first Arctic regionally E3SM configuration for ocean and sea-ice (E3SM-Arctic-OSI), employing data-based atmosphere, land, hydrology components. Our aim an improved representation coupled state, variability trends, exchanges mass property fluxes between sub-Arctic. We find that E3SM-Arctic-OSI increases realism simulated conditions compared similar low-resolution simulation without regional refinement (E3SM-LR-OSI). particular, through main gateways greatly respect E3SM-LR-OSI. Other aspects, such as freshwater content also satisfactorily simulated. Yet, other features, upper-ocean stratification thickness distribution, further improvements, involving either more advanced parameterizations, tuning, or additional grid refinements. Overall, offers E3SM-LR-OSI, at fraction (15 %) comparable configurations, permitting lower-latitude oceans cannot be directly accounted models.
منابع مشابه
The force balance of sea ice in a numerical model of the Arctic Ocean
The balance of forces in the sea ice model of Hibler [ 1979] is examined. The model predicts that internal stress gradients are an important force in much of the Arctic Ocean except in summer, when they are significant only off the northern coasts of Greenland and the Canadian Archipelago. A partition of the internal stress gradient between the pressure gradient and the viscous terms reveals th...
متن کامل15: An Arctic Ice/Ocean Coupled Model with Wave Interactions
– further our understanding of the hydrodynamical interactions between polar oceans and sea ice, especially with regard to the marginal ice zone (MIZ), i.e. the typically 10–100 km wide m ́elange of ice floes that connects open sea to the interior pack ice; – model the attenuation and spreading of directional seas within and in the waters adjoining MIZs, using a conservative, multiple wave scatt...
متن کاملAn Arctic Ice/Ocean Coupled Model with Wave Interactions
– further our understanding of the hydrodynamical interactions between polar oceans and sea ice; – develop new theoretical models and numerical methods with applications to other areas of science; – model attenuation and directional wave propagation within and in the waters adjoining the marginal ice zone (MIZ), using the conservative multiple wave scattering approach in a medium with random ge...
متن کاملArctic Ocean sea ice volume: What explains its recent depletion?
[1] Various observations and model results point to an arctic sea ice cover that was extraordinarily thin in the 1990s. This thin ice cover was caused by a strengthened cyclonic circulation of wind and ice and by unusual warmth of springtime air temperatures. Here modeled sea ice volume is decomposed into two components: first, a dynamic or wind-forced response to interannually varying winds bu...
متن کاملOn the future navigability of Arctic sea routes: High-resolution projections of the Arctic Ocean and sea ice
The rapid Arctic summer sea ice reduction in the last decade has lead to debates in the maritime industries on the possibility of an increase in cargo transportation in the region. Average sailing times on the North Sea Route along the Siberian Coast have fallen from 20 days in the 1990s to 11 days in 2012– 2013, attributed to easing sea ice conditions along the Siberian coast. However, the eco...
متن کاملذخیره در منابع من
با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید
ژورنال
عنوان ژورنال: Geoscientific Model Development
سال: 2022
ISSN: ['1991-9603', '1991-959X']
DOI: https://doi.org/10.5194/gmd-15-3133-2022