东南极洲冰芯中更温暖的间冰期的证据
L C Sime1, E W Wolff, K I C Oliver
1British Antarctic Survey, Cambridge CB3 0ET, UK. lsim@bas.ac.uk
Nature
|November 20, 2009
概括
南极冰芯记录显示,过去的冰期间温度明显高于此前估计的温度. 同位素特征与温度之间的关系是非线性的,这表明以前的估计可能过低.
科学领域:
- 古气候学 古气候学
- 冰川学的冰川学
- 气候建模气候模型
背景情况:
- 南极冰芯提供了关于过去80万年来气候变化的关键数据.
- 稳定的同位素比率 (氧和) 用于重建南极温度.
- 之前的研究假设同位素比和温度之间存在统一和恒定的关系.
研究的目的:
- 重新评估东南极冰芯中同位素特征与温度之间的关系.
- 调查这种关系在不同地点和不同气候时期的不均性.
- 为了完善过去的温度重建,特别是在冰河间时期.
主要方法:
- 分析了三份340公里的东南极冰芯记录.
- 整合通用循环模型 (GCM) 模拟.
- 同位素数据与模拟气候输出数据的比较.
主要成果:
- 温度和同位素特征之间的关系在温暖的间冰期期间在东南极冰芯地点之间有很大的差异.
- 南极东部冰的同位素组成表明,在温暖的气候下,对温度变化的敏感性降低.
- 这表明非线性转换对于在某些地点准确的温度重建是必要的.
结论:
- 以前对冰河间时期的温度估计可能被低估了.
- 南极冰川间气温的峰值可能至少比今天的温度高6K.
- 这些发现需要修订的方法来利用冰芯数据重建过去的南极气候.
相关概念视频
Global Climate Change
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
Isothermal Processes
A thermodynamic process that occurs at constant temperature is called an isothermal process. Heat slowly flows into the system or out of the system to maintain thermal equilibrium. Processes involving phase changes like water evaporation into steam or freezing water into ice at a constant temperature are examples of Isothermal Processes.
An ideal gas can also undergo isothermal expansion or compression.
For example, consider 1 mole of an ideal gas inside an isolated cylinder at initial volume V...
An ideal gas can also undergo isothermal expansion or compression.
For example, consider 1 mole of an ideal gas inside an isolated cylinder at initial volume V...
Phase Transitions: Melting and Freezing
Heating a crystalline solid increases the average energy of its atoms, molecules, or ions, and the solid gets hotter. At some point, the added energy becomes large enough to partially overcome the forces holding the molecules or ions of the solid in their fixed positions, and the solid begins the process of transitioning to the liquid state or melting. At this point, the temperature of the solid stops rising, despite the continual input of heat, and it remains constant until all of the solid is...
Effects of Temperature on Free Energy
The spontaneity of a process depends upon the temperature of the system. Phase transitions, for example, will proceed spontaneously in one direction or the other depending upon the temperature of the substance in question. Likewise, some chemical reactions can also exhibit temperature-dependent spontaneities. To illustrate this concept, the equation relating free energy change to the enthalpy and entropy changes for the process is considered:
The Fossil Record
The fossil record documents only a small fraction of all organisms that have ever inhabited Earth. Fossilization is a rare process, and most organisms never become fossils. Moreover, the fossil record only exhibits fossils that have been discovered. Nevertheless, sedimentary rock fossils of long-lived, abundant, hard-bodied organisms dominate the fossil record. These fossils offer valuable information, such as an organism's physical form, behavior, and age. Studying the fossil record helps...
The Evidence for Evolution
Genetic variations accumulating within populations over generations give rise to biological evolution. Evolutionary changes can result in the formation of novel varieties and entire new species. These changes are responsible for the diverse forms of life inhabiting the planet. The evidence for evolution suggests that all living organisms descended from common ancestors.The collection of fossils within sedimentary rocks give a record of common ancestry and often depicts the history of evolution.


