Ocean heat content and Earth's radiation imbalance

被引：14

作者：

Douglass, David H. ^{[1
]}

Knox, Robert S. ^{[1
]}

机构：

[1] Univ Rochester, Dept Phys & Astron, Rochester, NY 14627 USA

来源：

PHYSICS LETTERS A | 2009年 / 373卷 / 36期

关键词：

Climate; Radiative imbalance; Ocean heat content; DECADAL VARIABILITY; CLIMATE; PACIFIC; TEMPERATURE; BUDGET;

D O I：

10.1016/j.physleta.2009.07.023

中图分类号：

O4 [物理学];

学科分类号：

0702 ;

摘要：

Earth's radiation imbalance is determined from ocean heat content data and compared with results of direct measurements. Distinct time intervals of alternating positive and negative values are found: 1960-mid-1970s (-0.15), mid-1970s-2000 (+0.15), 2001-present (-0.2 W/m(2)), and are consistent with prior reports. These climate shifts limit climate predictability. (C) 2009 Elsevier B.V. All rights reserved.

引用

页码：3296 / 3300

页数：5

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[2] Comment on "Ocean heat content and Earth's radiation imbalance. II. Relation to climate shifts"
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