A few weeks ago, the U.S. Coast Guard announced it would begin to monitor the Arctic in a new way.
It’s called an “anemometer” and it measures atmospheric pressure.
The U.K. also plans to install its own instruments in the area to measure the atmosphere’s pressure.
But what does an anemometer actually do?
It’s a measurement device that measures the amount of carbon dioxide in the air.
And it’s not a very simple instrument.
For the past several decades, a lot of people have been using a method called radiative transfer theory to measure carbon dioxide levels in the atmosphere.
The theory says that as CO2 in the upper atmosphere increases, it heats the lower atmosphere, causing the atmosphere to become more reflective.
This causes the water vapor in the water to rise.
And as the water in the lower layer vaporizes, the CO2 is released.
That’s why it looks like the water is reflecting more sunlight.
But the theory also predicts that as the CO 2 in the stratosphere heats up, the water molecules in the higher layer will condense, making them more reflective and therefore less reflective of the sunlight.
In fact, this has been observed in the Antarctic and it’s been happening for hundreds of years.
In order to measure this, the instruments the U, U. K. and Australia use to measure CO 2 levels are called “anEMOs.”
These instruments measure the amount and temperature of water vapor.
But because they measure the air’s temperature, they don’t have to deal with the atmosphere, which is much hotter.
AnEMOs are also quite expensive, about $200,000 to $300,000.
And they are only meant for measuring CO 2 concentrations in the deep ocean, which means they can only measure the atmospheric pressure over a short period of time.
So what’s the difference between an anEMO and a measurement instrument?
A measurement instrument is a device that has a sensor in it that measures an air mass.
A lot of them measure CO2.
They can measure a lot.
They measure how much CO 2 is in the sky and what the temperature is.
The anEMOs can measure CO 3 levels, which can be measured in a couple of different ways.
They have a pressure sensor in them that measures CO 2 and the other one can measure the temperature of the air, which also is measured in the troposphere.
An anEMo measures the air in the ocean.
It doesn’t have a temperature sensor, so it can’t measure the temperatures of the water.
The AnEMO can measure how many molecules of water the atmosphere contains, which determines the pressure of the ocean, the pressure in the Earth’s crust, the temperature, and the water temperature.
An AnEMo also measures the temperature at a specific depth in the earth’s crust.
Because the anEMos measure the pressure, they can also measure the depth of the oceans below it.
So they can measure different types of atmospheric conditions, such as the amount or the temperature and the depth.
They also measure pressure, pressure gradients, the surface tension and so on.
And the Anemos can also calculate the velocity of the earth.
So, you have these measurements, you know, of the atmosphere and you know the pressure and the temperature.
But you don’t really know the depth, because you don, you don.
And this is one of the reasons why you don-the anEMoS can’t actually measure the velocity.
The instrument is not a good proxy for the depth because the pressure changes so quickly.
And there’s another problem, too, that an Anemo can’t record.
The pressure is very low.
But in the sea, there are lots of different types and sizes of things that move and interact with each other.
And a lot changes when the water changes.
And when the pressure goes down, there’s an interaction between the water and the pressure.
That creates some kind of feedback.
So the pressure is a very good proxy, but it can only tell you the velocity that the water moves through the ocean at a given depth.
That pressure depends on the depth that the anemo is at, which varies.
So it’s a very important thing to have an instrument that can measure that pressure.
It can tell you, for instance, the amount that’s moving and the speed of the object moving through the sea at a certain depth.
And that gives you a really good idea of the amount, or the speed, of that movement.
So you can’t really measure that directly.
So we have an AnEMOS and a standard measurement instrument, but they are both really expensive and difficult to use because they’re very difficult to operate.
But there is another way that they can do it that’s less expensive.
They’re able to measure how the temperature