HUSCAP logo Hokkaido Univ. logo

Hokkaido University Collection of Scholarly and Academic Papers >
低温科学研究所  >
雑誌発表論文等  >

MAIC-2, a latitudinal model for the Martian surface temperature, atmospheric water transport and surface glaciation

フルテキスト
Greve_etal_2010_PSS.pdf327.63 kBPDF見る/開く
この文献へのリンクには次のURLを使用してください:http://hdl.handle.net/2115/43084

タイトル: MAIC-2, a latitudinal model for the Martian surface temperature, atmospheric water transport and surface glaciation
著者: Greve, Ralf 著作を一覧する
Grieger, Björn 著作を一覧する
Stenzel, Oliver J. 著作を一覧する
キーワード: Mars
Planetary ice
Obliquity
Ice cap
Polar layered deposits
Ice age
発行日: 2010年 5月
出版者: Elsevier
誌名: Planetary and Space Science
巻: 58
号: 6
開始ページ: 931
終了ページ: 940
出版社 DOI: 10.1016/j.pss.2010.03.002
抄録: The Mars Atmosphere-Ice Coupler MAIC-2 is a simple, latitudinal model, which consists of a set of parameterisations for the surface temperature, the atmospheric water transport and the surface mass balance (condensation minus evaporation) of water ice. It is driven directly by the orbital parameters obliquity, eccentricity and solar longitude (Ls) of perihelion. Surface temperature is described by the Local Insolation Temperature (LIT) scheme, which uses a daily and latitude-dependent radiation balance. The evaporation rate of water is calculated by an expression for free convection, driven by density differences between water vapor and ambient air, the condensation rate follows from the assumption that any water vapour which exceeds the local saturation pressure condenses instantly, and atmospheric transport of water vapour is approximated by instantaneous mixing. Glacial flow of ice deposits is neglected. Simulations with constant orbital parameters show that low obliquities favour deposition of ice in high latitudes and vice versa. A transient scenario driven by a computed history of orbital parameters over the last 10 million years produces essentially monotonically growing polar ice deposits during the most recent 4 million years, and a very good agreement with the observed present-day polar layered deposits. The thick polar deposits sometimes continue in thin ice deposits which extend far into the mid latitudes, which confirms the idea of “ice ages” at high obliquity.
資料タイプ: article (author version)
URI: http://hdl.handle.net/2115/43084
出現コレクション:雑誌発表論文等 (Peer-reviewed Journal Articles, etc)

提供者: Greve Ralf

 

本サイトに関するご意見・お問い合わせは repo at lib.hokudai.ac.jp へお願いします。 - 北海道大学