00:00that exists in the atmosphere of the planet Earth, so if there was no
00:06efeito estufa, the temperature would be very less than it is today, but
00:11within the composition of the atmosphere, there are some gases that
00:15potentialisam this efeito estufa, so like the vapor of the water, for example,
00:20is an example that we feel like it is more common to us
00:28to feel the effects, because, like, who didn't say that,
00:33now, today, it's abafado, it's abafado because of the vapor
00:37of the water that there is a lot, so this efeito estufa
00:40is potentialized. And, along the years,
00:44it was perceived that there are some other gases that
00:48potentialisam this efeito estufa, and gases that
00:51accumulate, not like the vapor of the water that
00:54transform into the atmosphere, into the hydrologic.
00:57So, there are other gases that they
01:00will be accumulating, which are the gases emit
01:03by combustibles fósseis, right?
01:06So, we take the carbon, the carbon carbon,
01:10that is there, in the profundities,
01:13in the fundo of the ocean, and we come and
01:16that we put it in the atmosphere.
01:18This gas, he remains in the atmosphere and
01:19it is one of the potentialisors of the
01:25efeito estufa that, by consequence,
01:30will cause유ge global.
01:32So, I think it's more or
01:34that's the situation.
01:36And then the fact of the global warming means that we will have more energy in the atmosphere.
01:44The atmosphere will absorb more radiation from the Sol, and this energy, because on the planet everything has results,
01:57everything is interligated and has results.
02:00So, this energy that is left on the planet Earth will be transformed into extreme phenomena.
02:10So, this is the basic theory of the global warming.
02:14So, we are already experiencing many extreme phenomena,
02:19secas, chuva very intense, a frio very intense,
02:26so, all this is potential for the global warming.
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