Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1175/JCLI-D-16-0223.1 |
A Stochastic Dynamical Model of Arctic Sea Ice | |
Moon, Woosok1,2; Wettlaufer, J. S.3,4,5,6 | |
2017-07-01 | |
发表期刊 | JOURNAL OF CLIMATE |
ISSN | 0894-8755 |
EISSN | 1520-0442 |
出版年 | 2017 |
卷号 | 30期号:13 |
文章类型 | Article |
语种 | 英语 |
国家 | England; USA; Sweden |
英文摘要 | The noise forcing underlying the variability in the Arctic ice cover has a wide range of principally unknown origins. For this reason, the analytical and numerical solutions of a stochastic Arctic sea ice model are analyzed with both additive and multiplicative noise over a wide range of external heat fluxes Delta F-0, corresponding to greenhouse gas forcing. The stochastic variability fundamentally influences the nature of the deterministic steady-state solutions corresponding to perennial and seasonal ice and ice-free states. Thus, the results are particularly relevant for the interpretation of the state of the system as the ice cover thins with Delta F-0, allowing a thorough examination of the differing effects of additive versusmultiplicative noise. In the perennial ice regime, the principal stochastic moments are calculated and compared to those determined from a stochastic perturbation theory described previously. As Delta F-0 increases, the competing contributions to the variability of the destabilizing sea ice-albedo feedback and the stabilizing longwave radiative loss are examined in detail. At the end of summer the variability of the stochastic paths shows a clear maximum, which is due to the combination of the increasing influence of the albedo feedback and an associated "memory effect,'' in which fluctuations accumulate from early spring to late summer. This is counterbalanced by the stabilization of the ice cover resulting from the longwave loss of energy from the ice surface, which is enhanced during winter, thereby focusing the stochastic paths and decreasing the variability. Finally, common examples in stochastic dynamics with multiplicative noise are discussed wherein the choice of the stochastic calculus (Ito or Stratonovich) is not necessarily determinable a priori from observations alone, which is why both calculi are treated on equal footing herein. |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000403096200014 |
WOS关键词 | CLIMATE MODEL ; HEAT-TRANSPORT ; RADIATION ; FEEDBACK ; OCEAN |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/19761 |
专题 | 气候变化 |
作者单位 | 1.Univ Cambridge, Dept Appl Math & Theoret Phys, Cambridge, England; 2.British Antarctic Survey, Cambridge, England; 3.Yale Univ, New Haven, CT USA; 4.Univ Oxford, Math Inst, Oxford, England; 5.Royal Inst Technol, NORDITA, Stockholm, Sweden; 6.Stockholm Univ, Stockholm, Sweden |
推荐引用方式 GB/T 7714 | Moon, Woosok,Wettlaufer, J. S.. A Stochastic Dynamical Model of Arctic Sea Ice[J]. JOURNAL OF CLIMATE,2017,30(13). |
APA | Moon, Woosok,&Wettlaufer, J. S..(2017).A Stochastic Dynamical Model of Arctic Sea Ice.JOURNAL OF CLIMATE,30(13). |
MLA | Moon, Woosok,et al."A Stochastic Dynamical Model of Arctic Sea Ice".JOURNAL OF CLIMATE 30.13(2017). |
条目包含的文件 | 条目无相关文件。 |
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