Most global warming projection models correctly estimate the climate impact of the atmospheric processes, but often disregard the delayed feedback effects of the oceans. The laws of process control teach us that in order to correctly predict the future behavior of a process, any process, one must consider its totality, including the time constants, capacities and delayed feedback effects of its component sub-processes. In this column I will focus on these poorly understood or neglected sub-processes that are yet to take place in the oceans and will cause serious errors in the present global warming estimates.
Oceans cover 70% of our planet (more than 360 million km2). They absorb 90% of the total solar heat received and also absorb more than a quarter of the carbon dioxide we emit. The mass of the oceans is more than a thousand times greater than the atmosphere (1.3 x 1021 kg vs, 5.5 x 1018 kg) and has a much higher inertia. The top few meters of the ocean store as much heat as the planet’s entire atmosphere.
Solar radiation penetrates only the top 100-m layers. The water below is not directly heated. The water cycle on the earth (Figure 1) is started by the sun warming the surface of the oceans and causing the water to evaporate. This increases the water vapor content of the atmosphere, which increases the rate off water circulation. This cycle provides fresh water for the planet, while evaporation cools the oceans. The energy obtained travels with the water vapor until released in the process of condensation precipitation.
An increase in global warming and the resulting increased rate of evaporation influence the water cycles in the oceans. The common global warming models accurately consider the response of the atmospheric processes to the rise of global warming, but they often do not take into account the oceanic ones. So, I will focus on these often neglected oceanic processes, describing both the vertical and the horizontal "ocean conveyor belts."
The vertical ocean conveyor belt:
- Global warming increases the water vapor content of the atmosphere. When it condenses, it becomes the fresh water supply of the planet. Evaporation requires heat, which is taken from the ocean, thereby cooling it. Increased evaporation increases the rate of water circulation on earth by 7% per each °C temperature rise.
- The cooling caused by evaporation increases the density of the surface waters, making them heavier than the waters below. This causes the so called "thermohaline circulation," because as the warm surface waters are moved downward they force the cold waters below to rise. This circulation indirectly heats those layers that solar radiation cannot reach directly.
- As evaporation removes fresh water from the ocean's surface, so the remaining water becomes saltier (and therefore heavier) than the waters below. This process also increases the vertical circulation of the ocean's water, because as the saltier and warmer surface waters move downward, they heat the water layers below.
This "vertical water circulation" that brings heat to the lower levels is reduced as global warming increases. The increase causes the temperature of the surface waters to rise, reducing their density relative to that of the waters below. Therefore, if the density of the evaporating surface waters drop, the weight difference between that and the waters below drops, and this vertical circulation slows or eventually stops. The faster density increases with depth, the slower the vertical circulation becomes. As a result, less mixing takes place among the water layers, increasing global warming at the ocean's surface because it reduces the rate at which heat is transported down into the lower layers and more of it remains on the surface.