Tristan Gooley

I said, well, that's the only big dark place that will be warm enough to create the thermal that they'll look for. So it's, as I say, all wind is high pressure to low pressure. But what I'm trying to do is encourage people to not just think this is about these huge, massive, massive kind of charts we see on TV or internet forecasts.

This is something that's happening within, you know, 50 feet of us every day.

This is something that's happening within, you know, 50 feet of us every day.

This is something that's happening within, you know, 50 feet of us every day.

It's always trying to equal out, but actually air is a bit more viscous than most people think. Everyone sort of imagines that it could kind of equalize in five seconds. But it's more treacly than people imagine. It can't move across the surface of the earth as fast as people might think it does. But also, the second it equals out somewhere, the sun will create a difference somewhere else.

It's always trying to equal out, but actually air is a bit more viscous than most people think. Everyone sort of imagines that it could kind of equalize in five seconds. But it's more treacly than people imagine. It can't move across the surface of the earth as fast as people might think it does. But also, the second it equals out somewhere, the sun will create a difference somewhere else.

It's always trying to equal out, but actually air is a bit more viscous than most people think. Everyone sort of imagines that it could kind of equalize in five seconds. But it's more treacly than people imagine. It can't move across the surface of the earth as fast as people might think it does. But also, the second it equals out somewhere, the sun will create a difference somewhere else.

So if it was nighttime for 10 days solidly, things would start to equal out. But obviously, that's not what we experience. So everywhere the sun, at any one moment, the sun is rising somewhere and it's setting somewhere else. The sun is sort of setting this game going the whole time.

So if it was nighttime for 10 days solidly, things would start to equal out. But obviously, that's not what we experience. So everywhere the sun, at any one moment, the sun is rising somewhere and it's setting somewhere else. The sun is sort of setting this game going the whole time.

So if it was nighttime for 10 days solidly, things would start to equal out. But obviously, that's not what we experience. So everywhere the sun, at any one moment, the sun is rising somewhere and it's setting somewhere else. The sun is sort of setting this game going the whole time.

Every time things start to equalize a little bit, there'll be the sun heating up a bit of land more than the sea or heating up the low latitudes more than the high latitudes. So it's all driven by the sun. And because it's sunny somewhere always, the game never ends.

Every time things start to equalize a little bit, there'll be the sun heating up a bit of land more than the sea or heating up the low latitudes more than the high latitudes. So it's all driven by the sun. And because it's sunny somewhere always, the game never ends.

Every time things start to equalize a little bit, there'll be the sun heating up a bit of land more than the sea or heating up the low latitudes more than the high latitudes. So it's all driven by the sun. And because it's sunny somewhere always, the game never ends.

Dew and frost are related. And they're both a sign that we've had clear skies overnight, similar to we were talking about fog a little bit earlier. And it's a similar thing that if you have clear skies overnight, the heat leaves the land. I think everybody's comfortable with the idea that heat energy radiates from the sun to us.

Dew and frost are related. And they're both a sign that we've had clear skies overnight, similar to we were talking about fog a little bit earlier. And it's a similar thing that if you have clear skies overnight, the heat leaves the land. I think everybody's comfortable with the idea that heat energy radiates from the sun to us.

Dew and frost are related. And they're both a sign that we've had clear skies overnight, similar to we were talking about fog a little bit earlier. And it's a similar thing that if you have clear skies overnight, the heat leaves the land. I think everybody's comfortable with the idea that heat energy radiates from the sun to us.

But people are slightly less familiar with the way heat radiates out of everything, including us. You know, I'm looking at a desk and a chair. There's heat radiating out of those. I've got a cup of tea. There's heat radiating out of that. And heat radiates out of the land and it does it much, much more quickly and dramatically when there are clear skies.

But people are slightly less familiar with the way heat radiates out of everything, including us. You know, I'm looking at a desk and a chair. There's heat radiating out of those. I've got a cup of tea. There's heat radiating out of that. And heat radiates out of the land and it does it much, much more quickly and dramatically when there are clear skies.

But people are slightly less familiar with the way heat radiates out of everything, including us. You know, I'm looking at a desk and a chair. There's heat radiating out of those. I've got a cup of tea. There's heat radiating out of that. And heat radiates out of the land and it does it much, much more quickly and dramatically when there are clear skies.

So what we tend to find is if you've got the blanket, the stratus type cloud over an area at night, you wake up in the morning and there'll be no dew.