Video 1.2: Introduction to the Earth's climate system

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En provenance du cours de University of Manchester

Our Earth: Its Climate, History, and Processes

91 notes

University of Manchester

Our Earth: Its Climate, History, and Processes

91 notes

Develop a greater appreciation for how the air, water, land, and life formed and have interacted over the last 4.5 billion years.

À partir de la leçon

Building Blocks of Earth’s Climate System

Video 1.0: Introduction and Philosophy7:45

Video 1.1: How does science work?6:21

Optional Video: How do scientific papers get published?10:50

Video 1.2: Introduction to the Earth's climate system8:49

Video 1.3: How do we measure geologic time?9:50

Video 1.4: Geological Time Scale Song2:50

Video 1.5: Minerals and Rocks2:59

Video 1.5.1: Igneous Rock3:03

Video 1.5.2: Sedimentary Rock6:15

Video 1.5.3: Metamorphic Rock5:39

Video 1.6: Using radioactivity to date rocks - Dr. Ray Burgess7:48

Video 1.7: Using stable isotopes to understand Earth processes - Dr. Ray Burgess6:15

Video 1.8: How do we know how old the Earth is?5:46

Video 1.9: What are those rocks doing lying around?10:48

Rencontrer les enseignants

Prof. David M. Schultz
Professor of Synoptic Meteorology
School of Earth, Atmospheric and Environmental Sciences
Dr Rochelle Taylor
Postdoctoral Research Associate
School of Earth, Atmospheric & Environmental Sciences
Dr Jonathan Fairman
Postdoctoral Research Associate
School of Earth, Atmospheric and Environmental Sciences

Hi, my name is David Schultz.

Welcome back to Our Earth, it's climate, history, and processes.

Today, what we're going to learn is about the Earth's climate system.

And the first thing that I want to talk about are the five components of

the climate system.

The biosphere, the atmosphere, the lithosphere, the cryosphere, and

the hydrosphere.

So let's go through each one of these individually, shall we?

The biosphere.

This includes all life, plants, animals, single celled organisms on the earth,

in the water, on the earth's surface, and in the air.

There is the atmosphere.

This is the gaseous envelope that surrounds the earth.

This includes not only the gasses themselves and their chemical composition,

but other substances that are suspended in the atmosphere.

The liquid water droplets, the ice particles that comprised clouds and

precipitation as well as dust particles and

other aerosol particles that are suspended in the air.

There is the lithosphere this comprises the upper part of the earth's

surface maybe down to a few tens of kilometers, deep from the Earth's surface.

It doesn't include the deepest parts of the Earth's mantle.

But that's for a different topic.

We have the cryosphere.

This includes everything that's frozen on the Earth's surface.

We have the polar caps.

We have glaciers in the mountains.

We have sea ice and the permafrost, the frozen soils in the Arctic region.

And we have the hydrosphere,

this includes all the water substance on the earth in it's liquid form.

So, primarily the oceans, and any fresh water in lakes, rivers, and ground water.

The next thing we need to talk about is how these different spheres interact.

And for that I want to introduce the concept of forcing and response.

So when we talk about climate forcings and climate responses you'll know what I mean.

You can kind of think of this as cause and

effect with the forcings being the causes of something and

the effect being the change that results in the earth's climate system.

So here let me give you some examples that may help explain that.

When we look at causes these are,

as I mentioned external forcings to the earth's climate system.

These are plate tectonics, motions of the continents

on the surface of the earth being driven by processes deep within the earth.

We have orbital changes, changes to the orbit of the earth around the sun.

We have changes in solar input as the sun goes through its evolution,

it will change how much solar energy we receive on the planet.

And I've also included anthropogenic or manmade external forcings on the climate.

In this case I've excluded man from the biosphere to emphasize the changes

that we have made to the climate and how that might lead to some type of response.

So, these changes, these external forcings then go through

the earth's climate system to produce changes in vegetation or

the distribution of life on the planet.

Lead to changes in the chemical composition or

the dynamics, the motion of the atmosphere.

Changes in the land surface, as mountains rise up, as surfaces weather away.

Changes in the ice coverage and depth and volume of ice that we have on the planet,

as well as changes to the ocean, not only the chemical composition of the ocean, but

also changes in the circulation.

So it's useful to think of external forcing and

internal responses when we talk about a climate system.

This leads to another concept when we talk about forcing and response.

And that is, the idea of a feedback.

And we're going to talk about two different types of feedback.

The first one being positive feedback.

This is a process internal to the earth's climate that acts

to enhance the original action.

So in other words if I

make a change then this change will be amplified as the climate responds.

Here's an example, we call it the water-vapor feedback.

The idea here is that if the Earth's air temperature increases,

then the atmosphere has a greater capacity to incorporate water vapor into it.

This will lead to an increase in evaporation putting more water vapor

in the air and as we'll see water vapor is a greenhouse gas

this will lead to a increase in the air temperature.

So the idea here is that the positive feedback the that through

the positive feedback, the initial increase in

air temperature will put more water vapor in the air, which will lead to

a further increase in water vapor increase in the air temperature.

And this is the positive feedback.

An initial increase leads to a further increase.

Compare that to a negative feedback.

This is a process that counteracts the original action.

So here, we have the example of a cloud feedback.

Where if we increase the air temperature of the atmosphere, that again will

lead to an increase in evaporation, which will put more water vapor in the air.

More water vapor in the air means that it's more likely that clouds will

be formed.

This increase in the clouds may lead

to more reflection of incoming solar radiation.

And with less solar radiation reaching the surface of the earth, then we

will lead to a decrease in the atmospheric air temperature near the surface.

So, in this case, the negative cloud feedback of an initial

increase in temperature leading to a decrease in temperature offsetting that.

So, through these different feedbacks, we see that

the climate system can evolve in certain ways.

As illustrated by these two specific examples, an increase in air

temperature leading to more evaporation and more water vapor in the air,

we don't necessarily know which is going to win out.

And it may be that the positive feedback wins out in certain areas of the globe or

in certain conditions.

And the negative feedback wins out in other situations.

So, these feedbacks can be pretty complex.

They may be interacting, and they may be off-setting each other.

So, but I want to introduce these terms because we're

going to use them as we go through the course.

So, to summarize this lecture, we have the five components of the Earth's system,

the biosphere, atmosphere, lithosphere, cryosphere, and hydrosphere.

We've introduced the concept of climate forcing, and

responses, the cause and effect of how climate can change over time.

And then, we introduced the concept of positive and negative climate feedbacks.

And specifically, gave you some examples of how this works.

And told you that, you know, sometimes, they may offset each other, and

it may not be clear which climate process is dominate in any given situation.

So, thanks for listening, and I'll see you in the next video.

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