Paleoclimate - Was the medieval warm period global?

被引：220
作者：
Broecker, WS [1 ]
机构：
[1] Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY 10964 USA
来源：
SCIENCE | 2001年 / 291卷 / 5508期
关键词：
D O I：
10.1126/science.291.5508.1497
中图分类号：
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号：
07 ; 0710 ; 09 ;
摘要：
[No abstract available]
引用
收藏
页码：1497 / 1499
页数：3
相关论文
共 21 条
[1]  
Bond GC, 1999, GEOPH MONOG SERIES, V112, P35
[2]   Paleocean circulation during the last deglaciation: A bipolar seesaw? [J].
Broecker, WS .
PALEOCEANOGRAPHY, 1998, 13 (02) :119-121
[3]   A possible 20th-century slowdown of Southern Ocean deep water formation [J].
Broecker, WS ;
Sutherland, S ;
Peng, TH .
SCIENCE, 1999, 286 (5442) :1132-1135
[4]  
CLOW G, COMMUNICATION
[5]   Swiss glacier recession since the little ice age: Reconciliation with climate records [J].
Greene, AM ;
Broecker, WS ;
Rind, D .
GEOPHYSICAL RESEARCH LETTERS, 1999, 26 (13) :1909-1912
[6]  
Grove J. M., 1988, LITTLE ICE AGE, P1
[7]  
HOLZHAUSER H, 1997, ESF PROJECT EUROPEAN, V16, P35
[8]  
Hormes A, 1998, RADIOCARBON, V40, P809
[9]  
HORMES A, IN PRESS HOLOCENE
[10]  
HORMES A, 2001, 14C PERSPECTIVE GLAC, P176
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