相关实验视频
Updated: Jul 6, 2026

04:55
Using a Thermal Camera to Measure Heat Loss Through Bird Feather Coats
Published on: June 17, 2020
南极冬季热带层的显著变暖
J Turner1, T A Lachlan-Cope, S Colwell
1British Antarctic Survey, Natural Environment Research Council, Cambridge CB3 0ET, UK. j.turner@bas.ac.uk
概括
发现了南极冬季显著的热层变暖,比地球上任何其他区域变暖都要大. 这种30年每十年0.5-0.7°C的变暖趋势是基于新的南极放射探测器数据.
科学领域:
- 大气科学 大气科学
- 气候科学 气候科学
- 南极气象学 南极气象学
背景情况:
- 南极热层的热趋势尚未得到充分理解.
- 之前的研究缺乏南极冬季的全面数据.
研究的目的:
- 为了调查南极冬季热带层中未经记录的变暖.
- 量化观察到的温度变化的速度和意义.
主要方法:
- 对最近数字化和质量控制的南极无线电探测器观测结果的分析.
- 时间序列分析以评估过去30年的温度趋势.
主要成果:
- 在区域中热带气体中,统计学上显著的每十年升温趋势为0.50.7°C.
- 这种变暖比以前在全球范围内发现的任何区域热带层变暖都要大.
- 无线探测器数据证实了时间同质性,确保了数据可靠性.
结论:
- 已经确定了南极冬季热带层的未经记录的显著变暖.
- 根据目前的数据,这种变暖的原因仍未确定.
- 这一发现凸显了对南极气候动态的进一步研究的需要.
相关概念视频
Thermosensation
Peripheral thermosensation is the perception of external temperature. A change in temperature (on the surface of the skin and other tissues) is detected by a family of temperature-sensitive ion channels called Transient Receptor Potential, or TRP, receptors. These receptors are located on free nerve endings. Those detecting cold temperatures are closer to the surface of the skin than the nerve endings detecting warmth. These thermoTRP channels, while temperature selective, have relatively...
What is Climate?
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.
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.
Decreased Body Temperature
A decreased body temperature can occur in patients with hypothermia and frostbite. Heat loss with extended cold exposure overpowers the body's ability to create heat, resulting in hypothermia. Core temperature readings help classify hypothermia. Mild hypothermia is temperatures between 32 °C (89.6 °F) and 35°C (95 °F) and is caused by impaired thermoregulation. Moderate hypothermia is temperatures between 28 C (82.4 °F) and 32 °C (89.6 °F) caused by sustained extreme cold exposure, and severe...
Masonry in Cold and Hot Weather Conditions
In cold weather, masonry construction requires specific precautions to ensure mortar does not freeze before curing, as this can significantly weaken its strength and watertightness. Mortar temperature should be maintained between 60°F and 80°F to support proper hydration and curing. Below 40°F, mortar water must be heated, but should not exceed 120°F as high temperatures can reduce mortar's compressive and bond strength.
Other key practices include keeping masonry units and sand dry and...
Other key practices include keeping masonry units and sand dry and...
Boundary Layer Characteristics
When a fluid encounters a solid surface, a boundary layer forms due to the interaction between the fluid's motion and the stationary surface. This phenomenon is characterized by a thin region adjacent to the surface where viscous forces dominate, influencing the fluid's velocity profile. The development of the boundary layer begins at the leading edge of the surface and evolves as the fluid moves downstream.As the fluid flows over the surface, friction between the fluid and the wall slows down...

