相关实验视频
Updated: Jul 8, 2026

07:28
Evolution of Staircase Structures in Diffusive Convection
Published on: September 5, 2018
北大西洋的空间模式和热量变化的机制
M Susan Lozier1, Susan Leadbetter, Richard G Williams
1Division of Earth and Ocean Sciences, Nicholas School of the Environment and Earth Science, Duke University, Durham, NC 27708, USA. mslozier@duke.edu
概括
北大西洋在50多年中获得了热量,但区域冷却发生了. 通过北大西洋振荡指数测量的自然变化解释了这些海洋温度变化.
科学领域:
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
- 大气科学 大气科学
背景情况:
- 北大西洋在过去50年中吸收了大量的热量.
- 海洋变暖并非在所有地区均.
研究的目的:
- 为了研究北大西洋热量增长的区域差异.
- 了解观察到的海洋温度变化的驱动因素.
主要方法:
- 对整个盆地范围的热量流量数据的分析.
- 检查区域表面热量流变化的研究.
- 采用风力和浮力强迫的模型调查.
主要成果:
- 北大西洋显示盆地范围的热量增长为0.4 +/- 0.05 W/m^2.2.
- 热带和亚热带地区变暖了,而次极地区却变冷了.
- 区域热流变化明显大于盆地平均值,由北大西洋振荡指数解释.
结论:
- 风力和浮力强力的十年变化显著影响区域海洋温度.
- 北大西洋的强烈自然变化可能会掩盖人为变暖信号.
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.
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.
Mechanisms of Heat Transfer II
In convection, thermal energy is carried by the large-scale flow of matter. Ocean currents and large-scale atmospheric circulation, which result from the buoyancy of warm air and water, transfer hot air from the tropics toward the poles and cold air from the poles toward the tropics. The Earth’s rotation interacts with those flows, causing the observed eastward flow of air in the temperate zones. Convection dominates heat transfer by air, and the amount of available space for the airflow...
Mechanism of heat transfer
Understanding heat transfer mechanisms is essential for understanding how our bodies maintain balance in different environmental conditions. When the environment is thermoneutral, the body is in a state of balance, neither using nor releasing energy to maintain its core temperature. However, when the environment is not thermoneutral, the body employs four heat transfer mechanisms to maintain homeostasis: conduction, convection, evaporation, and radiation. These mechanisms facilitate heat...
Mechanisms of Heat Transfer
Heat transfer between the human body and its environment occurs through four main mechanisms: conduction, convection, radiation, and evaporation.
Conduction, accounting for approximately 3% of body heat loss at rest, is the process of exchanging heat between molecules of two materials in direct contact. This can result in both heat loss and gain. For instance, when the body is submerged in water, which conducts heat 20 times more effectively than air, it can either lose or gain significant heat.
Conduction, accounting for approximately 3% of body heat loss at rest, is the process of exchanging heat between molecules of two materials in direct contact. This can result in both heat loss and gain. For instance, when the body is submerged in water, which conducts heat 20 times more effectively than air, it can either lose or gain significant heat.
Mechanisms of Heat Transfer I
Just as interesting as the effects of heat transfer on a system are the methods by which the heat transfer occur. Whenever there is a temperature difference, heat transfer occurs. It may occur rapidly, such as through a cooking pan, or slowly, such as through the walls of a picnic ice box. So many processes involve heat transfer that it is hard to imagine a situation where no heat transfer occurs. Yet, every heat transfer takes place by only three methods: conduction, convection, and radiation.

