How to measure the temperature of the atmosphere

The measurement of the temperature on Earth is a complex process.

It involves a series of measurements called radiative transfer (RTP), which involves taking measurements of the radiative energy in the air and the resulting temperature.

A small amount of energy is transferred from the air to the earth, which then absorbs a small amount.

This radiative effect is known as the thermostat.

It’s a bit like measuring the temperature at your house.

You measure the room temperature by measuring the radiatively transferred energy in air that comes into your house, and then you measure the thermo-temperature of that room.

The difference between the two is known by the formula, T T :E E : E E : T T .

The temperature is then calculated by subtracting the temperature from the RTP.

This can be done for most of the Earth’s surface, and is called surface-temperatures.

For most parts of the planet, surface-ttemperature is very accurate, but there are some regions where the measurements are not very accurate.

The Earth’s atmosphere is made up of particles called greenhouse gases, or HGs.

The greenhouse gases are part of the greenhouse effect, a powerful and complex process in which the Earth radiates energy from the sun to the atmosphere.

The radiative heat that radiates out from the Earth is the greenhouse gas’s energy.

The temperature at the Earth surface is also known as surface-T, which is a measure of the average temperature of Earth’s oceans.

So it’s easy to understand why we know the temperature.

But we don’t know the average of the air on the surface of the globe, which can vary from one place to another.

The atmosphere of the earth is also made up mainly of water vapor and a small quantity of carbon dioxide.

This makes up about 30% of the water vapor on Earth.

Carbon dioxide is an extremely strong greenhouse gas, with a warming effect that can increase the temperature by about 0.6°C every decade.

Because of the ocean’s water vapor, we can measure the average surface temperature on the ocean without measuring the total greenhouse gas.

The water vapor that makes up the atmosphere of our planet has an average of around 0.01 °C per decade.

When we measure the air temperature, we subtract the water vapour from the total carbon dioxide in the atmosphere and we get the average.

We can also measure the greenhouse gases in the greenhouse atmosphere, and that’s where we find out the average for each year.

This average temperature is called the average global surface temperature.

The average temperature, measured on the planet’s surface is called a mean global surface air temperature.

If the average world surface air temperatures are higher than the mean global average, that means that the world has warmed faster than the average climate change for the last 100 years.

This means that we have warmed faster in the past, and we’ve warmed faster now than we did in the last century.

If our average global air temperatures for the past 100 years were higher than for the same time period, the planet would be warming faster than today.

That’s because we’re emitting more CO2 than it took to build the planet in the first place.

CO2 is a greenhouse gas that is emitted from fossil fuels like coal, oil, and gas.

Some climate models project that emissions from fossil fuel combustion will rise as a result of climate change.

These models include the assumption that humans will be responsible for half of all greenhouse gas emissions, and the assumption is based on the assumption of continued rapid increases in CO2 emissions over the next few decades.

The global average global mean surface air surface temperature in January is around -4.4°C, which means that it has warmed by 0.5°C since the year 2000.

In the past century, the Earth has warmed about 2.2°C faster than in the year 2100.

So the average worldwide surface temperature for the current year is now about -4°F.

We know that the average average temperature for all of Earth is now around 0°F, which makes it very warm.

The amount of warming is very high, but we know that this is mostly because of the CO2 that we’re adding to the Earth atmosphere, which has increased over the past few decades as a consequence of greenhouse gas emission.

This warming has led to global sea levels rising, as well as some of the extreme weather events that we’ve seen.

What about global warming?

We know from climate models that if greenhouse gas concentrations continue to rise as projected, they will cause sea levels to rise faster than they have for the 20th century.

That means that sea levels will rise faster and faster as the oceans cool and become warmer.

Sea levels will then rise faster, leading to more intense storms and extreme weather.

What does this mean for cities?

When the oceans warm, the oceans heat.

That causes the surface to cool, and as a response, the sea level rises.

As a result, cities

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