在轨道时间尺度上,南极温度和局部太阳辐射的同步性
Thomas Laepple1, Martin Werner, Gerrit Lohmann
1Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany. thomas.laepple@awi.de
Nature
|March 4, 2011
概括
南极冰芯数据可能不支持米兰科维奇理论. 积雪的季节性偏差意味着当地的阳光照射,而不是北半球气候,可以解释南极的温度变化.
科学领域:
- 古气候学 古气候学
- 气候科学 气候科学
- 地质物理学 地质物理学
背景情况:
- 米兰科维奇理论假设北半球夏季阳光照射驱动轨道时间尺度上的全球气候变化.
- 南极的温度记录,几乎与北极夏季阳光照射相一致,已被引用为证据.
- 没有直接的机制将北半球阳光和南极气候联系起来.
研究的目的:
- 重新评估南极冰芯温度记录的解释.
- 调查南极气候重建中的潜在偏差.
- 为了确定当地的阳光照射能否解释南极的温度变化.
主要方法:
- 在南极冰芯中分析季节性积雪偏差.
- 使用"记录器"系统中偏差的当前估计.
- 将重建的南极温度与本地和北半球阳光照射数据进行比较.
主要成果:
- 南极冰芯温度记录显示,由于季节性积雪,南极冬季偏向南极冬季.
- 这种偏差意味着当地的南极夏季阳光照射可以解释南极温度的轨道组成部分.
- 不需要援引与北半球气候的联系来解释观察到的南极温度模式.
结论:
- 来自南极冰芯的温度记录不是支持或反驳米兰科维奇假设的可靠指标.
- 解释过去的南极气候完全由北半球阳光照射驱动的解释可能是有缺陷的.
- 需要进一步的研究,以了解轨道时间尺度上的半球气候联系.
相关概念视频
What is Climate?
17.5K
Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
17.5K
Global Climate Change
24.4K
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.
24.4K
Temperature Measurement Sites
4.3K
A thermometer measures body temperature. The common sites for measuring body temperature are the oral cavity, axillary region, temporal artery, and skin surface, such as the forehead, abdomen, and axilla. True core body temperature is assessed in the rectum, tympanic membrane, pulmonary artery, esophagus, and urinary bladder.
Oral: When assessing oral temperature, the thermometer tip should be placed under the tongue in the posterior sublingual pocket. It offers accurate readings and can be...
Oral: When assessing oral temperature, the thermometer tip should be placed under the tongue in the posterior sublingual pocket. It offers accurate readings and can be...
4.3K
Thermometers and Temperature Scales
6.1K
Any physical property that depends consistently and reproducibly on temperature can be used as the basis of a thermometer. For example, volume increases with temperature for most substances. This property is the basis for the common alcohol thermometer and the original mercury thermometers. Other properties used to measure temperature include electrical resistance, color, and the emission of infrared radiation.
As many physical properties depend on temperature, the variety of thermometers is...
As many physical properties depend on temperature, the variety of thermometers is...
6.1K
Maxwell-Boltzmann Distribution: Problem Solving
2.3K
Individual molecules in a gas move in random directions, but a gas containing numerous molecules has a predictable distribution of molecular speeds, which is known as the Maxwell-Boltzmann distribution, f(v).
This distribution function f(v) is defined by saying that the expected number N (v1,v2) of particles with speeds between v1 and v2 is given by
This distribution function f(v) is defined by saying that the expected number N (v1,v2) of particles with speeds between v1 and v2 is given by
2.3K
Atomic Spectroscopy: Effects of Temperature
1.2K
Atomization, converting samples into gas-phase atoms and ions, is essential for atomic spectroscopy. The flame temperature required for atomization affects the efficiency of the atomic spectroscopic methods by increasing the atomization efficiency and the relative population of the excited and ground states.
At thermal equilibrium, the relative populations of excited and ground state atoms can be estimated using the Maxwell–Boltzmann distribution. For example, an increase in temperature...
At thermal equilibrium, the relative populations of excited and ground state atoms can be estimated using the Maxwell–Boltzmann distribution. For example, an increase in temperature...
1.2K


