*~*~Global Warming~*~*

-GLOBAL WARMING CONTINUED-

What can we do to help Earth?
The evidence that humans are causing global warming is strong, but the question of what to do about it remains controversial.
Even if we stopped emitting greenhouse gases today, the Earth would still warm by another degree Fahrenheit or so. But what we do from today forward makes a big difference.  Depending on our choices, scientists predict that the Earth could eventually warm by as little as 2.5 degrees or as much as 10 degrees Fahrenheit.

Is this possible?
Many people and governments are already working hard to cut greenhouse gases, and everyone can help!
Researchers at Princeton University have suggested one approach that they call "stabilization wedges." This means reducing Green House Gases emissions from a variety of sources with technologies available in the next few decades, rather than relying on an enormous change in a single area.  They suggest 7 wedges that could each reduce emissions, and all of them together could hold emissions at approximately current levels for the next 50 years, putting us on a potential path to stabilize around 500 ppm.
There are many possible wedges, including improvements to energy efficiency and vehicle fuel economy, and increases in wind and solar power, hydrogen produced from renewable sources, bio fuels (produced from crops), natural gas, and nuclear power.  There is also the potential to capture the carbon dioxide emitted from fossil fuels and store it underground—a process called "carbon sequestration."
In addition to reducing the gases we emit to the atmosphere, we can also increase the amount of gases we take out of the atmosphere.  Plants and trees absorb CO2 as they grow, "sequestering" carbon naturally.  Increasing forest lands and making changes to the way we farm could increase the amount of carbon we're storing.
Some of these technologies have drawbacks, and different communities will make different decisions about how to power their lives, but the good news is that there are a variety of options to put us on a path toward a stable climate!

www.environmentnationalgeographic.com

*~*~Global Warming~*~*

-GLOBAL WARNING-

What Causes Global Warming?

Scientists have spent decades figuring out what is causing global warming. The only way to explain the pattern is to include the effect of greenhouse gases emitted by humans.

One of the first things scientists learned is that there are several greenhouse gases responsible for warming, and humans emit them in a variety of ways-

The most come from the combustion of fossil fuels in cars, factories and electricity production. The gas responsible for the most warming is carbon dioxide, also called CO2. Other contributors include methane released from landfills and agriculture, nitrous oxide from fertilizers, gases used for refrigeration and industrial processes, and the loss of forests that would otherwise store CO2.

Different greenhouse gases have very different heat-trapping abilities. Some of them can even trap more heat than CO2. A molecule of methane produces more than 20 times the warming of a molecule of CO2. Nitrous oxide is 300 times more powerful than CO2. Other gases, such as chlorofluorocarbons, have heat-trapping potential thousands of times greater than CO2. But because their concentrations are much lower than CO2, none of these gases adds as much warmth to the atmosphere as CO2 does.

In order to understand the effects of all the gases together, scientists tend to talk about all greenhouse gases in terms of the equivalent amount of CO2. Since 1990, yearly emissions have gone up by about 6 billion metric tons of "carbon dioxide equivalent" worldwide, more than a 20% increase!

What effects does this have on Earth?
The planet is warming, from North Pole to South Pole, and everywhere in between. Globally, the mercury is already up more than 1 degree Fahrenheit (0.8 degree Celsius), and even more in sensitive polar regions. Signs are appearing all over Earth!

Some impacts from increasing temperatures are already happening.

• Ice is melting worldwide, especially at the Earth’s poles
• The decline of penguins on Antarctica have fallen from 32,000 breeding pairs to 11,000 in 30 years
• Sea level rise became faster over the last century.
• Some butterflies, foxes, and alpine plants have moved farther north
• Precipitation has increased across the globe
• Spruce bark beetles have boomed in Alaska and chewed up 4 million acres of spruce trees

Other effects could happen later this century, if warming continues-

• Sea levels are expected to rise between 7 and 23 inches
• Hurricanes and other storms are likely to become stronger
• Plants could bloom earlier than their pollinating insects become active
• Floods and droughts will become more common
• Less fresh water will be available
• Some diseases will spread, such as malaria carried by mosquitoes
• Ecosystems will change—some species will move farther north or become more successful; others won’t be able to move and could become extinct

www.environmentnationalgeographic.com

Global warming solutions...continued in my next blog

*~Sonic Boom~*

*~SONIC BOOM~*

What is it?

A shock wave caused by an object moving at supersonic speeds, heard as a loud boom!

 You can learn about sonic booms by looking at the wakes boats leave in the water.
If you toss a pebble in a pond, little waves will form in concentric circles and spread away from the point of impact.
If a boat travels through the pond at 3 to 5 miles per hour, little waves will propagate in the same way both ahead of and behind the boat, and the boat will travel through them.
If a boat travels faster than the waves can propagate through water, then the waves "can't get out of the way" of the boat fast enough, and they form a wake.
A wake is a larger single wave.
It is formed out of all the little waves that would have propagated ahead of the boat but could not.

When an airplane travels through the air, it produces sound waves.
If the plane is traveling slower than the speed of sound (700-750 mph), then sound waves can spread ahead of the plane.
If the plane breaks the sound barrier and flies faster than the speed of sound, it produces a sonic boom when it flies past.
The boom is the "wake" of the plane's sound waves.
All of the sound waves that would have normally spread ahead of the plane are combined together so at first you hear nothing, and then you hear the boom they create.
In conclusion, it is just like being on the shore of a smooth lake when a boat speeds past.
There is no disturbance in the water as the boat comes by, but eventually a large wave from the wake rolls onto shore.
When a plane flies past at supersonic speeds the exact same thing happens, but instead of the large wake wave, you get a sonic boom.

http://www.howstuffworks.com/

How is it created?

  -They are created mostly by objects traveling at speeds that exceed the speed of sound, known as Mach 1.

  -Mach is named after an Austrian physicist Ernst Mach who studied sound

  -Mach 2 travels at twice the speed of sound

FACTS

~Alaska Climate Continued~

ALASKA CONTINUED...

 
Daylight & Darkness in Alaska
From mid May to August, many Alaskans live in near constant daylight. When we lived in Fort Wainwright, we used to use black curtains to keep that sunlight out at night.
This phenomenon, known as the Midnight Sun, reaches as far south as Fairbanks and Anchorage.
Every year Fairbanks has a run called the Midnight Sun Run. The run begins at 10 pm  and finishes once everyone completes 6.2 miles. It was such a fun run! All the locals would gather and cheer you on & have water, powerade & fruit stands for you on the way!
As far as darkness goes in Alaska, at the very top of the state, there is a two-month winter period in which the sun doesn't rise. But that's the extreme, and winter's long nights get shorter the farther south you are in Alaska.  
 The winter's could seem gloomy, but there's fun things to do in the winter too. We attended an ice sculpture event where you can walk into houses made out of ice, sit on ice unicorns and even go on ice slides! You must take caution and wear the right clothing because colder seasons, can increase the danger of frostbite and hypothermia at low temperatures!

Alaska Snowfall Records!

Thompson Pass, a popular extreme ski and snowboard area north of Valdez, once received a record 974.5" of snow during the winter of 1952-1953.
Thompson Pass recorded 62" of snow during one single 24 hour period in December, 1955. In February of

The deepest recorded snow pack in Alaska, and the deepest in all of North America, occurred at Wolverine Glacier on the Kenai Peninsula during the winter of 1976-1977. The depth was 356". That's packed, condensed snow. Almost 30 feet deep!

Barrow, in the dry north, received a record minimum amount of snow during the winter of 1935-1936 of only 3".

Montague Island in 1976 received a record 332.29" of precipitation. That's almost an inch of rain per day!

Barrow received only 1.61" of precipitation during all of 1935.

Alaska stores an immense amount of fresh water in its glaciers. An amazing 75% of the world's fresh water is held in glaciers worldwide and Alaska holds more than its fair share.
Alaska has more than 5,000 glaciers, covering in excess of 100,000 square miles. Alaska has more glaciers than the entire rest of the world combined, excluding the ice fields of Antarctica and Greenland.

Alaska really is a memorable place to visit!

~Alaska Climate~

Alaska Climate

Alaska is our country's northern most state. It's above Canada and close to the North Pole.

When's the best time to visit Alaska?

Mid May to mid September is the preferred time to visit, with June-August being the best.
Not all of the state is as unbearable, cold and miserable year-round as a lot of people believe. Even if you don't have a lot of outdoor experience, guided tours allow you to discover true Alaska wilderness during the day. Whether you prefer to hike on an ice age glacier, explore the wilderness in a "bush" plane or take a dog sled ride, you'll find plenty of options to experience Alaska! The state's many famous rivers, lakes and protected coastal waters offer the chance to experience rafting, kayaking or jet boat rides. Also if you would like to see moose...Alaska is the place to be!


There are actually about six different climates-
1. The Fairbanks area has a wide range, with summers in the 70s-80s F or higher and winters far below 0 F.
2. The Anchorage region has summers in the range of 55-65 F and winters well below freezing.
3. Southeast Alaska-Juneau has summers in the 50s-60s F with mild winters that hover around the freezing mark.
4. The southwest is generally in the 50s F during the summer and below freezing in winter, coupled with lots of wind, snow, sleet and rain.
5. In eastern Alaska-along Canada's border, temperatures average about 60 F in the summer and about 10 to 14 F in winter.
6. Northern Alaska is cool to cold year round, with summer highs generally in the 40s-50s F and winter temperatures well below 0 F (similar to winter in Fairbanks).And just to confuse things, it can drizzle, fog over, gust mightily or chill out even during the peak of summer throughout the state. The climate is part of what makes Alaska such a magnificent place to visit!
Even though, no matter when you go, sweaters, warm clothing and rain gear will be useful.

~MONSOONS~

~MONSOONS~

Those of us who live in Arizona, likely know what to expect when the Arizona monsoon arrives.
Probably the most debated weather event in Arizona is our so called "monsoon". Just the word conjures up visions of rains and widespread flooding followed by heat and drought. The drastic wet/dry combination is the example that most of us learned about in school. However, the monsoon actually occurs in varying degrees, and in Arizona it's marginal, just not as intense as those found in other parts of the world.

DID YOU KNOW?

The term "monsoon" comes from the Arabic "mausim" meaning "season" or "wind shift."

WHAT IS A MONSOON?

A monsoon is a seasonal shift in the prevailing wind direction, that usually brings with it a different kind of weather.

The persistent wind flow is driven by a warm air mass with low pressure at the surface that forms over the continent as it is warmed by the sun.

Air from the relatively higher pressure air mass over the ocean flows toward the low pressure over land.

The most famous monsoon is the Indian summer monsoon, as it affects such a large portion of Asia. In May and June of each year, the dry northerly wind flow over India changes direction, and warm humid air from the Indian Ocean flows from the south, gradually overspreading the Indian subcontinent. Widespread torrential rains, and even severe thunderstorms, accompany the "onset" of the monsoon.

The Indian Ocean version of the hurricane, called a "cyclone", can also occur and move ashore in association with the onset of the monsoon. These cyclones have at times killed thousands of people who live in the low-lying areas along the eastern coast of India and Bangladesh.

A weaker version of this monsoon occurs over the normally dry southwestern United States like Arizona in the later summer when more humid air, accompanied by thunderstorms, invades the region.

WHEN DOES A MONSOON OCCUR IN ARIZONA?

Prior to 2008 the Arizona area monsoon was considered to have started when there were three consecutive days when the dew point averaged 55 degrees or higher. In 2008 the National Weather Service decided to take the guesswork out of monsoon start and end dates. After all, monsoon is a season, and most people should not be concerned with whether or not a particular dust storm was defined as monsoon storm or not. Beginning in 2008, June 15 will be the first day of monsoon, and September 30 will be the last day. Now we can be more concerned with monsoon safety and less concerned with definitions!

WHAT HAPPENS DURING A MONSOON?

Monsoon storms range from minor dust storms to violent thunderstorms. They can even spawn tornadoes, though that is very rare. Typically, Arizona monsoon storms start with heavy winds sometimes resulting in a visible wall of dust hundreds of feet high moving across the Valley. These dust storms are normally accompanied by frequent thunder and lightning often leading to heavy downpours. Monsoon rains average about 2-1/2", about 1/3 of our yearly rainfall.

SAFETY TIPS

WHILE DRIVING

-First SLOW DOWN
-Leave plenty of room between you and the vehicle ahead of you
-Watch carefully for water pooling on the roadway surface as this could cause your vehicle to slide or hydroplane.
-Do not enter an area where the roadway has been closed due to flooding!
-Drive with your headlights on and slowly
-Watch for blowing dust and if possible avoid driving into a dust storm
-If you choose to stop in a dust storm, do not stop on the roadway
-Make sure your vehicle is in good condition
-If you suffer a mechanical breakdown or tire failure, remain calm, slow down, keep the steering straight, and drive the vehicle to a safe area as far from traffic as possible
-ALWAYS wear your safety restraints

IF YOU ARE AT HOME

-Turn off all unnecessary power equipment to reduce the draw on power companies
-Keep batteries, flashlights, and a battery operated radio or TV handy
-Stay off the phone. Even cordless phones can cause a shock when lighting strikes nearby. Use cell phones only if necessary.
-Stay away from plumbing fixtures as lightning can travel along metal pipes.
-Keep away from windows as high winds can blow heavy debris.

 IF THE POWER GOES OUT 

-Switch off high usage items such as air conditioners, computers and televisions so there is no danger of overloading your system or damaging these products with voltage fluctuations when power returns.
-Surge protectors for your computer and electronic equipment will provide extra protection.
-Turn on your battery powered radio or TV for information
-Limit how often you open doors so cool air stays inside
-Keep your freezer and refrigerator door closed

 LIGHTNING

Lighting is dangerous no matter where you are. If you find yourself outdoors when lightning strikes:

-Seek shelter immediately
-Stay away from open fields, high land, trees, poles and standing bodies of water
-Do not swim or hold metal objects, including golf clubs and lawn chairs
-Once again stay off your phones and away from plumbing

Hurricanes cont.

HURRICANES CONTINUED...

The final stage is the hurricane stage!

Stage 4: Hurricane

Hurricanes have sustained one-minute winds of at least 74 mph, at an elevation of 10 meters. Winds in most hurricanes can become much stronger.

Hurricanes are categorized on a scale of 1 to 5 based on their wind speed, a scale known as the Saffir-Simpson hurricane wind scale, named after its originators, Herbert Saffir and Dr. Robert Simpson.

In developing tropical cyclones, strong thunderstorms occur. Air pressure drops at the surface of these storms. This low pressure attracts warm moist air from the ocean's surface. The Coriolis force causes the resulting low-level winds to spiral in a counterclockwise direction around the center of the low in the Northern Hemisphere, whereas winds swirl clockwise in the Southern Hemisphere.

Typically, an "eye" forms when the tropical cyclone reaches hurricane strength, but an eye is not necessary for a tropical cyclone to become a hurricane.

Another way to think of a hurricane is as a large heat engine. The fuel is moisture from warm ocean water. The moisture is converted to heat in the thunderstorms that form. Spiral rain bands that surround the tropical cyclone's core help feed the circulation more heat energy.

As air nears the center, it rises rapidly and condenses into clouds and rain. The condensation releases tremendous amounts of heat into the atmosphere. The result is lower surface pressure and strengthening winds.

In this way, the tropical cyclone's engine refuels itself, concentrating its power in a donut-shaped area, called the eye wall, surrounding the center. The eye wall typically contains the strongest surface winds.

Sinking air at the center clears the tropical cyclone of clouds and forms the "eye." Falling surface pressure can occur only if air mass is removed from the circulation center. This is accomplished by wind flowing away from the circulation in the upper atmosphere.

Thankfully with technology today, we have learned so much about hurricanes!

http://www.weather.com/

Hurricanes

HURRICANES

I have never witnessed a hurricane and I hope it stays that way! Hurricane comes from the Spanish word "huracan" which was inspired by Hunraken, the name for the ancient Mayan storm god or Hurakan, the Quiche god of thunder or any number of Caribbean terms for evil spirits or big winds. The word "hurricane" was first used to describe any localized tropical cyclone in the West Indies.

What is a hurricane?

A hurricane is defined as a tropical cyclone with sustained winds that have reached speeds of 74 mph or higher. These storms reach the status of "hurricane" only after strengthening over a period of days or even weeks.

Where do hurricanes form?

The process begins in the warm, moist air over the waters of the region known as the tropics, which includes the Gulf of Mexico, the Caribbean Sea, the eastern North Pacific Ocean and the North Atlantic Ocean. Tropical depressions, tropical storms, hurricanes, and typhoons are all tropical cyclones, and all may develop in this region.



Hurricane Katrina



What are the stages?

Before it can become a hurricane, a tropical cyclone must pass through four distinct stages:

Stage 1: TROPICAL DISTURBANCE

A tropical disturbance is a discrete system of clouds, showers, and thunderstorms that originates in the tropics and goes on for 24 hours or more.

Tropical waves are a type of tropical disturbance that develops about every four to five days, and some of these waves eventually strengthen to become tropical storms and hurricanes. Sometimes called easterly waves, they are areas of low pressure that move generally from east to west, embedded in the tropical easterly winds.

Stage 2: Tropical depression

When a tropical disturbance develops a closed circulation (counter-clockwise winds blowing around a center of low pressure in the Northern Hemisphere), it is designated as a tropical depression. Tropical depressions contain maximum sustained one-minute winds of 38 mph or less, at an elevation of 10 meters.

Stage 3: Tropical storm

A tropical cyclone is given a name by the National Hurricane Center once it reaches tropical storm status. Tropical storms have maximum sustained one-minute winds of 39-73 mph, at an elevation of 10 meters.

STAGE 4: THE HURRICANE STAGE IS CONTINUED IN MY NEXT BLOG...

http://www.weather.com/

*Hail*

Have you ever been in a hail storm?

Growing up in Montana I witnessed many hail storms. As kids we always thought they were fun! Sometime they weren't so fun. I remember one day we had to stay in the house because the hail came down so hard. The next day we came outside and a couple car windshields were cracked!

What is hail?

Hail is precipitation in the form of a chunk of ice that can fall from a cumulonimbus cloud. They are usually associated with thunderstorms and most hail falls from the central region of a cloud in a severe storm. 

How does hail form? 

Hail begins as tiny ice pellets that collide with water droplets.
The optimum freezing level for the formation of hail is from 8,000 to 10,000 feet.
The water droplets attach themselves to the ice pellets and begin to freeze as strong updraft winds toss the pellets and droplets back up into the colder regions of the upper levels of the cloud.
As the attached droplets freeze, the pellets become larger.
Both gravity and downdraft thunderstorm winds pull the pellets back down, where they encounter more droplets that attach and freeze as the pellets are thrown, once again, back up through the cloud.

Hailstones

The more times a hailstone is tossed up and down through the cloud, the larger the hailstone will be. Hailstones the size of softballs had many more trips up and down through the cloud than pea-sized hailstones.
Large hailstones are an indication of powerful updraft and downdraft winds within a thunderstorm. This is why large hail is associated with severe thunderstorms.
To create pea-size hail (about 1/2 inch in diameter) winds within the thunderstorm updraft will generally be around 20 miles per hour. Quarter size hail (3/4 of an inch in diameter) requires updrafts of about 40 miles per hour.
Golf ball size hail (1 3/4 inches in diameter) needs updrafts of around 55 miles per hour and softball size hail, approximately 100 miles per hour!
The largest hailstone ever measured in the United States fell at Coffeyville, Kansas, on September 3, 1970. It weighed 1.67 pounds and measured 17.5 inches in circumference.

Hail Alley
The Great Plains states, especially northeastern Colorado and southeastern Wyoming, receive more hail yearly than any other part of the United States. Hail in this area of the country is most likely to fall late in the afternoon during the months of May and June and is often responsible for extensive crop loss, property damage and livestock deaths.

http://www.weather.com/

Tornadoes

Have you ever witnessed a tornado?

While being stationed in Oklahoma, I witnessed a tornado! It was very scary! I remember we were woken up from sleeping outside and we were being yelled at to run to the bus! Seeing that tornado was unbelievable, the sky looked so unreal. We raced away to safety and thankfully no one was harmed. I never want to witness a tornado again. I will never live where there are tornadoes!

Tornado heart

What is a tornado?

A tornado is a violent rotating column of air extending between a cloud and the surface of the earth.
Tornadoes are usually formed by thunderstorms. Even though, they have been known to occur without the presence of lightning.
 

 

Tornado Facts

 
Tornado wind speeds are estimated on the damage they cause. Tornadoes are categorized on a scale of 0 (weakest) to 5 (strongest).
 
The United States has the highest incidence of tornadoes worldwide, with more than 1,000 occurring every year. This is due to the unique geography that brings together polar air from Canada, tropical air from the Gulf of Mexico, and dry air from the Southwest to clash in the middle of the country, producing thunderstorms and the tornadoes they spawn.
 
Tornadoes can come one at a time, or in clusters, and they can vary greatly in length, width, direction of travel, and speed. They can leave a path 50 yards wide or over a mile wide. They may touch down for only a matter of seconds, or remain in contact with the ground for over an hour.

When & Where are Tornadoes?

In the United States, "tornado season" is generally in the spring. Tornadoes usually occur April through July. May and June are the peak months. But like thunderstorms, tornadoes can form any time of the year.

The area in which tornadoes are most common is known as "tornado alley," typically defined the region from Texas north to Nebraska. Even though, tornadoes can and do occur in every state in the country.

http://www.weather.com/

'Rainforests'

'Weather in the Rainforest'

I have only witnessed rainforest weather while watching movies. The rain comes down so hard at times! While living here in Arizona, I feel like I would not mind that at times. We enjoy escaping the heat here in Yuma, Arizona and going to the Rainforest Cafe in Phoenix, Arizona!

What is a rainforest?


A rainforest is a dense, warm and wet jungle which has around 100 inches of rainfall every year. There is no dry season and rain falls nearly every day. 50% of the rainforest water comes from evaporation and the relative humidity is always high. The temperature in the rainforest is most likely to be hot and damp. The average temperature is 77 degrees F.



The rainforest is filled head to toe with lush green vegetation. Many trees in the rainforest have canopies on them, providing shade for the animals and plants. The canopies help shield the plants and animals from the scorching sunlight. The rainforests are very humid due to the warm sunlight, rain and the canopies shading over the plants keeps in the moisture.

The rainforest in the early morning

Where can you find a rainforest?

Rainforests can be found on every continent across the Earth, except Antarctica.

There is even an extinct rainforest in Castle Rock, Colorado.

Tropical rainforests are located in tropical regions, and temperate rainforests are found in higher latitude regions.

The major areas of tropical rainforests are in West Africa, South East Asia and South and Central America. The best known rain forests are found in tropical regions between the Tropics of Cancer and Capricorn.

Can you name 10 different rainforests?

1. The Tongass National Forest located in Southeastern Alaska - largest intact coastal temperate rainforest in the world


2. The Hoh Rainforest inside Olympic National Park, Washington- famous moss covered rainforest

3. Amazonia, also called the Amazon Rainforest - located within nine nations in the Amazon Basin of South America (Brazil, Colombia, Peru, Venezuela, Ecuador, Bolivia, Guyana, Suriname and French Guiana)

4. Lacandon jungle located in Chiapas, Mexico - Mexico's last remaining significant rainforest

5. Monteverde Cloud Forest in Costa Rica-This large reserve is one of the most outstanding wildlife sanctuaries in the Americas and includes eight distinct ecological zones

6. The Congo Rainforest - famous for its gorillas, chimpanzees, and elephants as well as its native population of forest dwellers known as pygmies. Rainforests in the Congo are disappearing faster than forests anywhere else in the world

7. Daintree Rainforest located in North Queensland Australia - The area is home to the greatest concentration of plant species that are rare, or threatened with extinction, anywhere in the world

8. Kayan Mentarang National Park in Kalimantan (Borneo), Indonesia - contains the largest unbroken stretch of protected rainforest in Borneo

9. Sagano Bamboo Forest in Kyoto, Japan-This bamboo forest is one of the most beautiful bamboo forest in Japan. In the 1870s when Edison was looking for a good bamboo as a material for his early light bulb, the governor of Kyoto recommended two sources of bamboo


10. Khao Sok National Park, Thailand - rainforest is 160 million years old and thought to be the oldest rainforest on Earth

rainforest waterfall

 Rainforests are disappearing every minute........so help take care of it!

Sandstorms

Oh no not a Sandstorm!

Those of us that live in Yuma, Arizona have all experienced some sort of sandstorm. I remember one day I looked in the sky and I thought I saw smoke from them burning the fields. It was not smoke! It was a sandstorm on its way. The sand in the sky is a site to see. That day I left for work and told someone to close the window in our kitchen. They forgot to close the window and when I got home there was sand everywhere in my kitchen! It was such a mess to clean up. I know now to close my windows myself!


What causes a sandstorm?


Sandstorms are caused by strong winds blowing over loose soil or sand. They pick up so much of that material that visibility is reduced. In desert regions at certain times of the year, sandstorms become more frequent. This happens because the strong heating of the air over the desert causes the lower atmosphere to become unstable. This instability mixes higher winds in the middle troposphere downward, producing stronger winds at the surface. I know some people refer to sandstorms as "dust storms".

Whoa!

Facts about sandstorms:

They can be seen as solid walls of sand that are up to 5,000 feet high.

Similar dust storms from wind borne particles can be found on the planet Mars.

In the United States of America, sandstorms are very rare due to the lack of large deserts, the development of proper agricultural techniques, and the common cloud cover, which will block out some of the sun's heat.

Deforestation, excessive cultivation of farmland, over-grazing and excessive use of water resources can cause sandstorms.

Special air filters can be installed in your car to prevent sand from getting into the engine.

In order to protect yourself from sandstorm you can wear protective goggles/suits.

In Kuwait, the month of April is known as 'sandstorm month'.

Sandstorms that come from Northern Africa and drift across Europe are called 'Sahara Sand Storms'.

Dust Bowl 1930

Problems caused by sandstorms:

A devastating sandstorm known as The Dust Bowl of the 1930s lasted about a decade. Its primary area of impact was on the southern Plains. The agricultural devastation helped to lengthen the Depression whose effects were felt worldwide.

Sandstorms can interfere with travel, and sometimes obliterates entire roads, and dry, flat regions, such as parts of the western United Sates.

Sand storms can cause hacking coughs, and the sand and dust have also been known to be capable of carrying 'infectious diseases'. Sand particles, unlike dust ones, will clog air passages, and cause the person who breathes them in to choke. Dust particles may simply cause an allergic reaction!




http://library.thinkquest.org/

*Blizzards*

*Woah! Bizzards*

While growing up in beautiful Montana I experienced many blizzards. I have driven in blizzards and let me tell you that was scary. You can only see a few feet in front of you during a blizzard. Let me also tell you that businesses don't always close just because there is a blizzard. I remember one day there was a blizzard and I still had to go to work. On the way to work I rear ended a car while breaking. It was icy! It wasn't that hard, but I did hit that car. The driver of the car I hit, didn't even care. He continued on as if nothing happened. I guess in Montana some just get used to that. Wow that sure does make me miss Montana! lol :)

This is what it looks like driving in a blizzard!

Here are some facts about blizzards-

 Blizzards happen when a low temperatures 20°F or lower are combined with winds that are at least 35 mph or greater.

There is also sufficient falling and/or blowing snow in the air that reduces visibility to 1/4 mile or less for a duration of at least 3 hours.

Severe blizzards have temperatures near or below 10°F, winds exceeding 45 mph, and visibility reduced by snow to near zero.


Storm systems powerful enough to cause blizzards usually form when the jet stream dips far to the south, allowing cold air from the North to clash with warm air from the South.


Colder and drier polar air brings atmospheric temperatures cold enough for the development of snow, sleet, or freezing rain.

After seeing this picture, I still miss Montana!

Where you can find blizzards-

The Rockies (beautiful Montana), Dakotas, Gulf of Mexico into Canada and parts of Minnesota are vulnerable to blizzards.


In the southern central Great Plains, rapidly intensifying low pressure systems moving out of the Rocky Mountains can cause heavy snows and strong winds to the north, while to the south and east are thunderstorms and rain.

http://www.weather.com/