FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3007970411> ?p ?o ?g. }

• W3007970411 endingPage "982" @default.
• W3007970411 startingPage "951" @default.
• W3007970411 abstract "Abstract. We compare the mass budget of the Arctic sea ice for 15 models submitted to the latest Coupled Model Intercomparison Project (CMIP6), using new diagnostics that have not been available for previous model inter-comparisons. These diagnostics allow us to look beyond the standard metrics of ice cover and thickness to compare the processes of sea ice growth and loss in climate models in a more detailed way than has previously been possible. For the 1960–1989 multi-model mean, the dominant processes causing annual ice growth are basal growth and frazil ice formation, which both occur during the winter. The main processes by which ice is lost are basal melting, top melting and advection of ice out of the Arctic. The first two processes occur in summer, while the latter process is present all year. The sea ice budgets for individual models are strikingly similar overall in terms of the major processes causing ice growth and loss and in terms of the time of year during which each process is important. However, there are also some key differences between the models, and we have found a number of relationships between model formulation and components of the ice budget that hold for all or most of the CMIP6 models considered here. The relative amounts of frazil and basal ice formation vary between the models, and the amount of frazil ice formation is strongly dependent on the value chosen for the minimum frazil ice thickness. There are also differences in the relative amounts of top and basal melting, potentially dependent on how much shortwave radiation can penetrate through the sea ice into the ocean. For models with prognostic melt ponds, the choice of scheme may affect the amount of basal growth, basal melt and top melt, and the choice of thermodynamic scheme is important in determining the amount of basal growth and top melt. As the ice cover and mass decline during the 21st century, we see a shift in the timing of the top and basal melting in the multi-model mean, with more melt occurring earlier in the year and less melt later in the summer. The amount of basal growth reduces in the autumn, but it increases in the winter due to thinner sea ice over the course of the 21st century. Overall, extra ice loss in May–June and reduced ice growth in October–November are partially offset by reduced ice melt in August and increased ice growth in January–February. For the individual models, changes in the budget components vary considerably in terms of magnitude and timing of change. However, when the evolving budget terms are considered as a function of the changing ice state itself, behaviours common to all the models emerge, suggesting that the sea ice components of the models are fundamentally responding in a broadly consistent way to the warming climate. It is possible that this similarity in the model budgets may represent a lack of diversity in the model physics of the CMIP6 models considered here. The development of new observational datasets for validating the budget terms would help to clarify this." @default.
• W3007970411 created "2020-03-06" @default.
• W3007970411 creator A5001566161 @default.
• W3007970411 creator A5007702365 @default.
• W3007970411 creator A5008553156 @default.
• W3007970411 creator A5014590879 @default.
• W3007970411 creator A5014998263 @default.
• W3007970411 creator A5016441101 @default.
• W3007970411 creator A5023166970 @default.
• W3007970411 creator A5025099373 @default.
• W3007970411 creator A5035789653 @default.
• W3007970411 creator A5042851193 @default.
• W3007970411 creator A5048343791 @default.
• W3007970411 creator A5058432419 @default.
• W3007970411 creator A5068168995 @default.
• W3007970411 creator A5069707078 @default.
• W3007970411 creator A5072426522 @default.
• W3007970411 creator A5081995463 @default.
• W3007970411 creator A5089357421 @default.
• W3007970411 creator A5089602850 @default.
• W3007970411 date "2021-02-24" @default.
• W3007970411 modified "2023-10-18" @default.
• W3007970411 title "An inter-comparison of the mass budget of the Arctic sea ice in CMIP6 models" @default.
• W3007970411 cites W1613849817 @default.
• W3007970411 cites W1863529719 @default.
• W3007970411 cites W1865372759 @default.
• W3007970411 cites W1964551106 @default.
• W3007970411 cites W1966431154 @default.
• W3007970411 cites W1976923042 @default.
• W3007970411 cites W1983349253 @default.
• W3007970411 cites W1986015116 @default.
• W3007970411 cites W1990701514 @default.
• W3007970411 cites W1996653992 @default.
• W3007970411 cites W2000869494 @default.
• W3007970411 cites W2006165291 @default.
• W3007970411 cites W2009412734 @default.
• W3007970411 cites W2015426195 @default.
• W3007970411 cites W2019314030 @default.
• W3007970411 cites W2031027346 @default.
• W3007970411 cites W2036366180 @default.
• W3007970411 cites W2038838351 @default.
• W3007970411 cites W2042862842 @default.
• W3007970411 cites W2051220568 @default.
• W3007970411 cites W2052697879 @default.
• W3007970411 cites W2054088207 @default.
• W3007970411 cites W2055688720 @default.
• W3007970411 cites W2056294409 @default.
• W3007970411 cites W2068359259 @default.
• W3007970411 cites W2078844631 @default.
• W3007970411 cites W2084461152 @default.
• W3007970411 cites W2093804327 @default.
• W3007970411 cites W2102140204 @default.
• W3007970411 cites W2103104092 @default.
• W3007970411 cites W2104713109 @default.
• W3007970411 cites W2126208974 @default.
• W3007970411 cites W2142130713 @default.
• W3007970411 cites W2144096669 @default.
• W3007970411 cites W2147737607 @default.
• W3007970411 cites W2151094192 @default.
• W3007970411 cites W2169372365 @default.
• W3007970411 cites W2233082033 @default.
• W3007970411 cites W2303915963 @default.
• W3007970411 cites W2336250479 @default.
• W3007970411 cites W2491031937 @default.
• W3007970411 cites W2510019860 @default.
• W3007970411 cites W2515336612 @default.
• W3007970411 cites W2548920327 @default.
• W3007970411 cites W2754310675 @default.
• W3007970411 cites W2766942317 @default.
• W3007970411 cites W2780318220 @default.
• W3007970411 cites W2787298971 @default.
• W3007970411 cites W2793379698 @default.
• W3007970411 cites W2801740427 @default.
• W3007970411 cites W2807209884 @default.
• W3007970411 cites W2808164051 @default.
• W3007970411 cites W2883803127 @default.
• W3007970411 cites W2885724302 @default.
• W3007970411 cites W2890288701 @default.
• W3007970411 cites W2897516365 @default.
• W3007970411 cites W2900373313 @default.
• W3007970411 cites W2925511745 @default.
• W3007970411 cites W2951290763 @default.
• W3007970411 cites W2953301534 @default.
• W3007970411 cites W2962764966 @default.
• W3007970411 cites W2969545894 @default.
• W3007970411 cites W2971199049 @default.
• W3007970411 cites W2982338710 @default.
• W3007970411 cites W2982625375 @default.
• W3007970411 cites W2998885490 @default.
• W3007970411 cites W3014962122 @default.
• W3007970411 cites W3017049878 @default.
• W3007970411 cites W3030446301 @default.
• W3007970411 cites W3045493740 @default.
• W3007970411 cites W3093306034 @default.
• W3007970411 cites W3107502106 @default.
• W3007970411 cites W4211257092 @default.
• W3007970411 doi "https://doi.org/10.5194/tc-15-951-2021" @default.
• W3007970411 hasPublicationYear "2021" @default.

• next