Averaged over Earth's surface, the 1993–2020 heat-gain rates were 0.37–0.41 Watts per square meter for depths from 0–700 meters (down to 0.4 miles), depending on which research group's analysis you consult. Meanwhile, heat gain rates were 0.15–0.31 Watts per square meter for depths of 700–2,000 meters (0.4–1.2 miles). For depths between 2000–6000 meters (1.2–3.7 miles), the estimated increase was 0.06 Watts per square meter for the period from June 1992 to July 2011. According to the State of the Climate 2019 report, "Summing the three layers (despite their slightly different time periods as given above), the full-depth ocean heat gain rate ranges from 0.58 to 0.78 W m -2 applied to Earth’s entire surface."
Additionally, clouds, water vapor, and greenhouse gases emit heat that they have absorbed, and some of that heat energy enters the ocean . Waves, tides, and currents constantly mix the ocean, moving heat from warmer to cooler latitudes and to deeper levels.
As water warms, it expands, so estimates for ocean temperature can be deduced from sea surface heights. To get a more complete picture of ocean heat content at different depths, scientists and engineers also use a range of in situ temperature-sensing instruments.
To get a more complete picture of ocean heat content at different depths, scientists and engineers also use a range of in situ temperature-sensing instruments. Among these are a fleet of more than 3,000 robotic “floats” that measure ocean temperature around the world. Known as Argo floats, the sensors drift through the ocean at different depths. Every 10 days or so, according to their programmed instructions, they rise through the water, recording temperature (and salinity) as they ascend. When a float reaches the surface, it sends its location and other information to scientists via satellite, and then descends again.
The heat energy eventually re-enters the rest of the Earth system by melting ice shelves, evaporating water, or directly reheating the atmosphere. Thus, heat energy in the ocean can warm the planet for decades after it was absorbed. If the ocean absorbs more heat than it releases, its heat content increases.
Water actually has one of the highest specific heat capacities of all the substances on Earth. Hydrogen gas, helium gas, and aqueous (liquid) ammonia are a few substances with a higher heat capacity than water .
Those in the water are most likely feeling cooler than those on the sand. This is due to the high specific heat capacity of water. In other words, the same amount of heat energy when applied to sand and water will increase the temperature of the sand more than it will increase the temperature of the water. Water actually has one of the highest ...
a) As ocean surface temperatures increase, the energy transferred to the atmosphere increases air temperatures. There is a lag time as the heat capacity of oceans release heat slowly. Land areas closest to the ocean receive more mild temperatures than areas farther inland. Warmer air temperatures may also increase precipitation as the air contains more moisture.
c) As ocean surface temperatures increase, the energy transferred to the atmosphere decreases air temperatures. There is no lag time as the heat capacity of oceans release heat slowly. Land areas closest to the ocean receive more dramatic temperatures than areas farther inland. Warmer air temperatures may also increase precipitation as the air contains more moisture.
Heat energy is released to the atmosphere as water vapor condenses to form water droplets around condensation nuclei (precipitation).
d) Water vapor and other greenhouse gases trap heat closer to Earth's surface, affecting weather patterns as the trapped warm, moist air rises and cools.
c) Relatively cooler surface air from the land moves away from the land to replace the warmer, rising air above the oceans.
a) The land loses its heat more quickly than water, resulting in relatively cooler air temperatures above the land during the evening.
a) Cooler air can hold more moisture than warmer air.
a. winds deflect to the right in the Northern Hemisphere.
Water can pile up higher than the edge of a container due to its low surface tension.
a. ocean salinity varies as a function of season.