An
earlier blog entry (The Many Faces of Climate) looked at climate in a
general way. When we talk about climate, what do we mean? There are
many answers, but simplest is the usual weather in an area. For
example, in the northern countries like Canada, Finland, Norway, and
Siberia it is quite cold much of the year. At the poles, Antarctica
and the Arctic, it's always cold. Then there are places that are
almost always warm like Guam or Hawaii. Places can have one to four
seasons. This is the temperature component of climate.
Climate
includes how much rain and snow occurs over a long period of time in
a specific area. Most people are familiar with places like the
Sahara Desert, where it rarely rains. There is a place in Chile that
is considered the driest on earth, the Atacama desert. It goes
without rain for 4 years or more at a time, and there may have been
one period of nearly 200 years without rain. In 2011, it both rained
and snowed there, a rare weather event that just happened to occur in
our lifetimes.
Mountain snow |
Snow
is the more common form of precipitation in high altitudes and some
of the more northern areas. In high altitudes, snow may stay on the
mountain top year round. Sometimes, glaciers form. Glaciers are not
as permanent as they may seem. Glaciers come and go at different
rates due in most part to the amount of snowfall, which builds up and
compresses to form ice. Some last for many years, some do not. For
a while, people were worried the Himalayan glaciers were melting (the
Himalayas are a mountain range in Asia). This could result in
flooding, especially if lakes were to break free and run down the
mountains. Also, people use the water which does naturally melt off
in the summer for a source of water. It turned out that measurements
with satellites showed there was no serious melting and some of these
glaciers may even be growing. Sometimes scientists report things
either without enough checking first or later on, better ways to
measure things come along. And we find out our planet is not all
that fragile.
High wind |
Climate
also includes wind, how much sun places have on average and how much
humidity there is. Places around the equator tend to be sunny.
Places like England have a lot of rain and thus a lot of humidity.
There are places with 40 mile an hour winds and places with gentle
breezes.
Wind combined with drought |
What
affects climate? Many, many things. In later posts, we will write
about some of these things. Does climate change? Of course.
Nothing stays the same. Sometimes climate changes quickly and
sometimes it takes million of years. People have been very good at
adapting to many of these changes. If the world gets warmer, we
adapt. If it gets colder, we adapt. We can move around and/or build
better shelters and find more efficient ways to produce food.
Sometimes it's not easy, but we have managed.
We
study climate so we can learn about how it works and maybe be able to
predict a few things in the future. Predicting changes in the
climate is not easy. Most of the time, we have to just build our
homes stronger, or higher, and grow whatever food works well in the
area. We can build where floods are not so common or elevate our
homes in case of floods. Since we can buy food, fuel, clothing and most anything else we cannot produce in one place from some other place in the world,
regional weather events don't have the effects that the Dust Bowl and
the Little Ice Age did. Climate has always included floods,
tornadoes, hurricanes, sunshine, warm weather and cold weather.
There are few, if any, places on earth where the weather/climate is
always ideal.
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