Sunday, November 7, 2010

Module VI - Atmospheric Systems Introduction
























NASA Photo Credit Apollo 17 Dec. 7, 1972



Essential Question:
How are
the Earth, atmosphere and cultures all connected?

Introduction:

At the beginning of the previous module, it was suggested that the ocean serves to demonstrate how everything on Earth is connected. This notion can be taken a step further;
Because the atmosphere covers 100% of Earth's surface, it is arguably the best example of how on Earth everything is connected.

Like our
fluid ocean, our fluid atmosphere flows around and over all surfaces and physical obstacles without regard for political boundary or culture. It can be thought of as our most common resource on Earth. Common in the sense that we all share it, and whatever happens to and within it is shared by all in common.

In a sense, we're like lobsters living at the bottom of an immense ocean of air, trying to understand the invisible medium in which we dwell, usually obliviously.

Scientific study, starting with balloons and ending with satellites, has revealed its complex structure, including some surprising extremes in radiation, temperature, density and composition.

But let's not be fooled by the apparent enormity of this great envelope of gases. Early pictures of our planet taken from space gave us our first dramatic glimpse into how thin and ephemeral this gauze of gases truly is.

Scientifically, we will explore
the composition, structure and dynamics of the atmosphere, with an eye toward how it participates in the thermodynamics of Earth's heating and cooling processes. There's even a lab on the phun physics of phase.

Culturally, we will explore some of the more recent discoveries regarding the atmosphere's role in distributing and concentrating airborne
anthropogenic pollutants, along with the disproportionate impacts borne by arctic people.


Saturday, November 6, 2010

Module VI - Cultural Connections








ENGAGE

Cultural Connections

We've discussed how Earth's ocean helps regulate our planet's temperature by moving its excess heat in vast
currents from where it's hot to where it's not, namely from the equator to the poles.

As we will learn in subsequent segments of this module, this is even more so for the atmosphere. And like the ocean, there is an unfortunate passenger that hitches along with the atmosphere for its cross-country ride - industrial pollution.

Along the way, industrial pollutants end up in the food web, concentrating from the
bottom-up as they move poleward. As these dangerous compounds enter the food web, they bio-accumulate each step of the way, concentrating at higher latitudes primarily in the fats of arctic mammals - the blubber of seals and whales among others that arctic people have been consuming to survive for thousands of years.

The fall-out in the Arctic from industrialized societies
at lower latitudes are the industrial pollutants released from modern factories. The list includes heavy metals, PCBs and POPs and everything else in between. These dangerous chemicals are rafted toward the poles aboard the ocean and atmospheric currents that carry them from lower to higher latitudes.

It is ironic and tragic that the more densely populated western industrialized societies at lower latitudes that are most responsible for atmospheric pollution have such a detrimental impact on those who live in the sparsely populated, minimally developed arctic regions.

It is doubly ironic that those who are the least culpable for creating pollution and who live closest to the land and subsist most directly from their immediate environment, are most at risk for suffering the effects of industrial pollution.


EXPLORE

Teachers' Domain
Watch these two TD videos that explain the mechanisms that cause the
Contaminants in the Arctic Food Chain and the Arctic Haze that threatens the arctic ecosystem and those who live there.

Contaminants in the Arctic Food Chain





Arctic Haze






YouTube
Here's another resource describing research efforts to understand the causes and implications of Arctic pollution is this YouTube video,
NASA ARCTAS Mission, produced by NSERCTV -- The National Suborbital Education and Research Center

NASA ARCTAS Mission






EXPLAIN
  • Why are dangerous pollutants accumulating disproportionately in the Arctic?
  • What vectors are responsible for transporting pollutants to the Arctic?
  • How does bio-accumulation occur?
EXTEND
  • Research the risks of nursing infants in the arctic.
EVALUATE

  • What are the responsibilities of industrialized societies regarding the impacts of pollution rafted elsewhere?



ENGAGE

Career Connections
Ever adapting, Alaska Natives embrace the use of new technologies to provide food, shelter, safety and transportation in a harsh and demanding environment. This could reasonably be said of all cultures, but the extremes of the Arctic environment and the remoteness of Native villages raises the stakes and brings the use of new technologies into sharper focus.


EXPLORE

Teachers' Domain
Let's take a few minutes to explore a lofty career that is vital across the vast distances of Alaska,
Alaska Native Pilots.

Alaska Native Pilots






EXPLAIN
  • Why is aviation so important in Alaska?
  • What are some of the unique perils Alaskan aviators face?
  • Describe how Alaska Native pilots merge their traditional knowledge with western science.
EXTEND
  • What digital resources would be useful to a bush pilot?

EVALUATE
  • What are the proper roles of new digital technologies in the context of Native Ways of Knowing?

Friday, November 5, 2010

Module VI - The View from Space

EXPLORE

NASA
How better to launch an exploration of global systems than with NASA? There are thousands of images and resources you can discover and use at the NASA National Space Science Data Center. And while you're there, click around the NASA image resources library for images that interest you. Maybe there's one there for your next lesson or blog response.


Google Earth
While we're getting the BIG picture on global weather systems, let's take some time to visit Google Earth to see what NASA's Weather Layer has to show us with this near real time data.

Download this layer from the Google Earth gallery of free plug-ins and open it in Google Earth. But remember, this large program works better if you don't have too many layers open at the same time. You may want to turn the weather layer off when you're using other Google Earth features.






EXPLAIN
  • What does the Google Earth Weather Layer show you about weather patterns across the globe?
EXTEND
  • Take a screen shot or two to include in your blog that illustrates an atmospheric phenomenon you've learned about.
  • What are some ways you could use this kind of near-real time weather information?
EVALUATE

  • What is the value of Google Earth and NASA information and imagery for today's digital learners?

Thursday, November 4, 2010

Module VI - Atmospheric Structure and Dynamics










ENGAGE

Our atmosphere is a complex cocktail of molecular and atomic gases from Nitrogen to Neon, though in vastly differing concentrations. And because of their differing weights, temperatures and associated densities, these gases array themselves in stratified layers not too unlike the layers in the ocean we discussed earlier.

After all, the ocean and the atmosphere are both fluid in their behavior, and are therefore able to easily move and sort themselves by density differences. However, the atmosphere has some peculiarities in pressure and temperature that are not at all like the ocean.



EXPLORE

Teachers'Domain
Explore these two TD interactive resources,
Vertical Structure of the Atmosphere and Compare and Contrast Warm and Cold Air Front .

Helpful Hint: While you're at it, click on the State Standards associated with these resources. It's all right there in TD. And its so easy to use.


Vertical Structure of the Atmosphere








Compare and Contrast Warm and Cold Air Fronts






EXPLORE SOME MORE...

National Geographic
Besides, surfing the ocean and surfing the web, did you know we can also su
rf the atmosphere. This YouTube - hosted National Geographic video narrated by Dr. Iain Stewart is a fun and engaging way to Reveal Earth's Atmosphere.


Reveal Earth's Atmosphere

Check out National Geographic for other more Dr. Iain Stewart and other great cultural and geoscience resources.



EXPLAIN
  • Why are the four major layers of the atmosphere separated as they are?
  • What causes the increased temperature in the stratosphere?
  • Can planes fly in the mesosphere? Why or why not?
  • On what does the temperature in the thermosphere depend?

Helpful Hint: These four questions came right from the Teachers' Domain interactive resources linked to,
Vertical Structure of the Atmosphere. Can you find them?


EXTEND

  • What resources or ideas do you have to help students visualize their invisible atmosphere?

EVALUATE

  • What are the practical values of Teachers' Domain and National Geographic digital resources for your professional purposes?



Wednesday, November 3, 2010

Module VI - Wind and Weather










ENGAGE

Convection and Heat Flow in the Atmosphere - More Hot Air...
Most of us can think of an example from our daily life that demonstrates convection. Whether it's the warmer water near the surface of the lake we're swimming in, or the greater warmth near the ceiling compared to the floor, we've all learned that heat rises.

And as we discussed on the previous module on ocean circulation, cold, denser fluids descend. So much of what we discussed regarding density driven ocean circulation applies to the atmosphere as well. But instead of the ocean currents, here we'll explore the atmospheric currents--wind.

In the atmosphere, the motions of rising and falling gases of differing temperature, humidity and densities create the winds which are further directed by the larger forces of Earth's rotation and corresponding Coriolus force.

In the atmosphere, there are two main causes for air density to decrease; Increased temperature and increased water vapor caused by evaporation both decrease the density of air and cause it rise.

As the water vapor-rich warm air rises, it also expands and correspondingly cools. This cooling permits water vapor to condense. This way the atmosphere releases heat high in the atmosphere that it gained through evaporation at the surface.

So, here we see one simple, but very powerful method in which our planet moves heat from where it's hot to where it's not; This convection driven evaporation-condensation system, called latent heat flux, accounts for 23% of Earth's net heat budget.

All these varied forces interact to create complex, but distinct and predictable patterns of wind, weather and climate around the globe. Let's explore some of the online resources the help us to visualize and better understand and appreciate weather, whether or not you're a meteorologist.

EXPLORE

Teachers' Domain
Here's a TD animated video resource that demonstrates how the physics principles we have been exploring are coupled in the inseparable interface between the ocean and atmosphere; Ocean Temperatures and Climate Patterns.

And the TD-hosted NOVA interactive resource, Giving Rise to The Jet Stream, illustrates nicely the complexities of the interacting forces that create Earth's weather.

The Jet Stream and Horizontal Temperature Gradients is another TD interactive resource that helps to demonstrate how different forces interact to create the weather patterns that are distinct to various regions.



Ocean Temperatures and Climate Patterns





Giving Rise to The Jet Stream





The Jet Stream and Horizontal Temperature Gradients


EXPLAIN
  • What are some of the differences in winds and weather associated with latitude on Earth?
  • How do temperature differences between the poles and equator (thermal gradient) affect wind velocities in the Jet Stream?
  • What forces work together to create the Walker Cell?
EXTEND

  • Why is it difficult to discuss weather apart from the role of the ocean?
EVALUATE
  • How do these TD digital resources serve to enhance student learning?


EXPLORE SOME MORE...

YouTube
From YouTube, here are some of the basics presented as the Six Principles of How Weather Works, by Weather School. A more technical and informative YouTube video, Global Circulation, shows graphically where and how the patterns of weather occur across the planet.

And just try not to be mesmerized by this amazing composite of a year's worth of satellite data showing water vapor motion across the planet; Water Vapor Circulation on Earth.





EXPLAIN
  • What is the primary force that causes weather?
  • How does the differential heating of the planet contribute to wind and weather patterns?
  • How do the seasons affect the position and behavior of the atmospheric circulation cells?
  • What role does Earth's rotation play in creating wind and weather?
EXTEND
  • Monitor the atmosphere over Alaska by satellite in near-real-time. A picture's worth a thousand words.
  • For the more scientifically ambitious, try NASA's Atmospheric Science Data Center for lots of great information and resources.

EVALUATE

  • What resources so far have been the most engaging for you? Your students?


Tuesday, November 2, 2010

Module VI - Phun Physics










ENGAGE

Phun Physics of Phase Change - Blab....
There are common experiences in our daily lives that reveal methods employed by heat's restless nature to move from where it's hot to where it's not. Shivering outside the shower while dripping wet is one example. Complaining about the August heat in New Orleans invariably leads to matter-of-fact statements to the effect that, "it's not the heat, it's the humidity."

Let's boil this down, so to speak. You certainly know by now that water exists most commonly in nature in three phases or states: solid, liquid and vapor. You also certainly understand the relative thermal energy level, or heat differences of each of these phases; ice is cold (low thermal energy) and vapor is hot (high thermal energy) and liquid is somewhere in between.

But did you know that movement between each of these phases requires a substantial exchange of energy that does not change the temperature of water one bit?

That's why boiling water on the stove can't get any hotter than 100 degrees Celsius. All the thermal energy moving into the water at that temperature can only cause evaporation because evaporation at the surface of water removes heat from water at the same rate as the heat is added.

Or we could condense it all just by saying, evaporation is a cooling process. Huh?

You'll recall from our last module that water has a high heat capacity--that water requires 1 calorie per gram to change the temperature 1 degree Celsius.

Water also has a high latent heat of vaporization. This is the amount of thermal energy required to break all the hydrogen bonds that hold water together in its liquid state. This value registers at a whopping 540 calories per gram!

Which is to say that 1 gram of water at 100 degrees Celsius requires the input of an additional 540 calories of thermal energy to change phase from liquid to vapor. No wonder you're shivering outside your shower with all that heat leaving your skin as water turns to vapor and drifts away--from where it's hot to where it's not.

The same numbers and processes hold true in reverse; water condensing from vapor to liquid releases 540 calories per gram. Stated another way, condensation is a warming process.

That's why steam is so dangerous. It's a double burn. First, it burns because of it's high temperature; Secondly, it burns again as it releases its latent thermal energy while changing phase from vapor to liquid.

And all this holds true for the other famous phase change, freezing--except for the numbers. The latent heat of fusion for water (freezing) comes in around 80 calories per gram. That is, 1 gram of solid water (ice) at 0 degrees Celsius requires an additional 80 calories of thermal energy to become 1 gram of liquid water at the same temperature.

Which is to say, like evaporation, thawing is a cooling process. That's why we put ice in our beverages. And just like the condensation process described above, freezing is a warming process.

This may sound strange, but water freezing in the arctic helps to warm the surrounding air as the water releases 80 calories of thermal energy per gram into its immediate environment. More cool information on ice to come in following modules.

Still Confused?
Here's the bottom line - Whenever water changes phase, whether melting, freezing, evaporating or condensing, thermal energy is always released or absorbed, depending on the direction of the change. In nature this energy either comes from, or is released into the environment depending, again, on the direction of the change.

EXPLORE
Phun Physics of Phase Change - LAB!
Let's try our hand at backwards design. Examine the graph and information. How would you design a lab to create similar results?

There are many simple labs that require little more than water and a thermometer to demonstrate these basic principles. Take a look around the net and find one that best suits your students.

Helpful Hint: Safety in the lab is always a real issue. Many seemingly simple labs hold real perils. From broken glass to bad burns, protect your students and yourself by understanding and employing authentic safety practices in your labs.






















EXPLAIN
  • What is the relationship between thermal energy and phase change in water?
  • How is this different from the thermal energy required to change temperature?
  • How do the phase changes of water help regulate Earth's temperature?
EXTEND
  • What other labs or demonstrations reveal the flow of thermal energy through systems?
EVALUATE

  • How valuable is an understanding the physics of phase change to understanding weather and climate?


ENGAGE

Life Under Pressure
We aren't surprised to hear about the tremendous pressure at the bottom of the ocean. It makes sense that the weight of all that water would have such an enormous effect. But it's oft said, we live at the bottom of an ocean of air with similar results.

The weight of the air on the surface of the Earth averages about 14.7 lbs per square inch. Or about 2100 lbs per square foot. Or about 42,0000 lbs of pressure on the surface of your body. But we don't notice it much unless we change altitude quickly in a plane or elevator.


Anybody who's watched a TV weather report knows that
atmospheric pressure plays an important role in determining the forecast; That is, pressure affects the behavior of wind and water vapor. Therefore atmospheric pressure also plays an important role in determining when and where heat is transferred in the atmosphere.

Before TV weather reports, our more agricultural forebears and mariners monitored this law of physics by watching their handy
barometer. They also utilized the power of this phenomenon by using pressure cookers to better preserve food. That is, by increasing the vapor pressure in a cooker, they could cook at higher temperatures.

Conversely, we have to cook food longer at higher altitudes because water boils at a lower temperature due to the decreased atmospheric pressure.

Low Pressure = Cloudy/Rain
Now, let's condense these concepts, so to speak. Reduced atmospheric pressure allows water vapor in the air to cool and condense into liquid more easily because reducing the pressure of a gas decreases its temperature.

As the water vapor condenses, it releases 540 calories per gram of thermal energy in to the atmosphere, thus warming it. (Interestingly, reduced atmospheric pressure also allows water to evaporate more easily because of its corresponding reduction in vapor pressure.
)

High Pressure = Clear/Sunny
Conversely, increased atmospheric pressure limits the condensation of water because increasing the pressure of a gas also increases its temperature. You might correctly predict here that an increase in atmospheric pressure limits water's evaporation by increasing its vapor pressure, just like in grandma's pressure cooker.

Helpful Safety Hint: Because of the affects of pressure on boiling water, the explosive results of removing the cap from an overheated car radiator should be universally understood and avoided.


EXPLORE

YouTube

Check out some of the more surprising effects of pressure on phase change.

This is a YouTube video produced by the
Edwards Vacuum Corporation, called Making Ice by Boiling Water. While you're there, see what related videos are posted.


Making Ice by Boiling Water






EXPLAIN
  • What is the relationship between evaporation, condensation, vapor pressure and atmospheric pressure?
  • Where does the energy to boil water in a vacuum come from?
  • Why does the water freeze? Where does the heat go?
EXTEND

  • What stories can you tell that relate to any of these scientific principles?
EVALUATE

  • How valuable is an understanding the physics of pressure to understanding weather and climate?

Monday, November 1, 2010

Module VI - Blog It!

Essential Question:
How are
the Earth, atmosphere and cultures all connected?

After you have reviewed all TD and YouTube resources and completed the Google Earth activities for this module, it's time to Blog It!


3 Questions

    1. Explain: What new learning or reflections have you taken from this module?
    2. Extend: How might you use this week’ information and resources in your lessons?
    3. Evaluate: How useful, insightful or relevant are this module’s information and resources?
3 Colleagues

  • Whose blogs did you visit this week?
  • Did you link to their blog?
  • What did you like?