Reconciling Bolling warmth with peak deglacial meltwater discharge

被引：22

作者：

Lohmann, G

Schulz, M

机构：

[1] Max Planck Inst Meteorol, D-20146 Hamburg, Germany

[2] Univ Kiel, Inst Geowissensch, D-24118 Kiel, Germany

来源：

PALEOCEANOGRAPHY | 2000年 / 15卷 / 05期

关键词：

D O I：

10.1029/1999PA000471

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

Paleoclimatic data indicate warm conditions during the Bolling period, whereas climate modeling studies predict significant cooling, triggered by the concomitant deglacial meltwater flux into the Atlantic Ocean. We suggest that the lack of an adequate representation of deep water flow over the Greenland-Scotland Ridge in ocean circulation models can account for this discrepancy.

引用

收藏

页码：537 / 540

页数：4

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