aleCcowaN
imperfecto del subjuntivo
im not convinced the heat left the system. but i admit, im totally ignorant about the geosphere's heat content.
Departing on the text you quoted, once you talked about the geosphere I had no idea what heat were you talking about. I always supposed you had used geosphere as a nick for lithosphere, as you mentioned hydrosphere and atmosphere separately. In what is traditionally called the energy budget of the Earth, some 45-47 TW are contributed by the planet's crust and mantle, about a 1/3500th of what we get from the Sun. You may imagine that heat to be radiated into space, but the system that accounts for most of it is what I explained: sea water radiates energy into space in the middle of the polars nights and dawns and ice is formed leaving a heavy brine at -1.8°C to dissolve in more cold water and sink as a cold downstream reaching the ocean bottom, a distributed stream that may amount at certain dates as much as 5 Sverdrups. That's why most of the sea water is between -2°C and 5°C, in spite of the inners of the planet to be white hot and the surface temperature to average 14°C. That part of the hydrosphere is the climatic anchor that avoids surface temperatures to make even crazier excursions for even longer times during "common" events like Toba-like eruptions, 1km-diametre meteorite impacts, methane clathates sacks bursts, or the original event of masses of biped apes fancying to drive fast and furious. But unlike those ephemeral mega-events, the apes continue to come and behave the same way.
If you were talking about other thing, be clear. Your two-line posts start to resemble those of denialists' here, verbal Rorschach tests thought more to elicit long replies, just for the fun of it, than to foster an exchange of ideas.
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