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What Is the Difference Between Weather and Climate?
It’s a sweltering midsummer day. “It must be global warming,”
mutters someone. But is it the Earth’s changing climate that has
made the day so warm? Or, is it just the weather that is so
unbearable?

Weather
Weather is the mix of events that happen each day in our
atmosphere including temperature, rainfall and humidity.
Weather is not the same everywhere. Perhaps it is hot, dry and
sunny today where you live, but in other parts of the world it is
cloudy, raining or even snowing. Everyday, weather events are
recorded and predicted by meteorologists worldwide.

Climate
Climate in your place on the globe controls the weather where
you live. Climate is the average weather pattern in a place over
many years. So, the climate of Antarctica is quite different than
the climate of a tropical island. Hot summer days are quite
typical of climates in many regions of the world, even without the
affects of global warming.
 The only type of severe       Called tornadoes over land
  weather event that we          and waterspouts over
                                 ocean, these wild weather
  name individually, these       events churn air at the
  are among Earth’s              fastest speeds ever recorded
  largest and fiercest           on Earth. While they are
  storms. Each storm is          often short-lived, often only
                                 existing for a few
  able to, for a week or         minutes, the intense winds
  more, travel thousands         and flying debris from
  of miles stirring              tornadoes can destroy
  seas, toppling                 everything in their path.
  trees, and leveling        
  buildings.
 Hurricanes and typhoons    Tornadoes and waterspouts
   These storms are common          Waking up in the morning
    in the spring and summer          to find a fresh white
    when there is warm air
    near the ground and cool          blanket of snow coating
    air above. Small                  the ground may be
    thunderstorms may only            commonplace in many
    exist for an hour while           areas, occurring several
    large Super cell storms can
    last for several hours            times each winter, yet it
    spawning                          remains an exciting
    tornadoes, hail, intense          surprise since predicting
    lightning, and flash              winter storms is not easy.
    flooding.
       Thunderstorms                        Blizzards
Climate encompasses the statistics of, atmospheric
pressure, wind, precipitation, atmospheric particle temperature,
humidity count and other meteorological elemental
measurements in a given region over long periods. Climate can
be contrasted to weather, which is the present condition of these
elements and their variations over shorter periods. A region's
climate is generated by the climate system, which has five
components: atmosphere, hydrosphere, cryosphere, land
surface, and biosphere. The climate of a location is affected by
its latitude, terrain, and altitude, as well as nearby water bodies
and their currents. Climates can be classified according to the
average and the typical ranges of different variables, most
commonly temperature and precipitation. Paleo climatology is the
study of ancient climates. Since direct observations of climate are
not available before the 19th century, paleo climates are inferred
from proxy variables that include non-biotic evidence such as
sediments found in lake beds and ice cores, and biotic evidence
such as tree rings and coral. Climate models are mathematical
models of past, present and future climates. Climate change may
occur over long and short timescales from a variety of factors;
recent warming is discussed in global warming.
A depression in geology is a landform sunken or depressed below the
surrounding area. Depressions may be formed by various
mechanisms.
Structural or tectonic related:
Structural basin: A circular, syncline-like depression; a region of
tectonic down warping ( associated with a subduction zone and
island arc);
Graben or rift valley: down dropped and typically linear depressions
or basin created by rifting in a region under tensional tectonic forces.
Pull apart basin caused by offset in a strike slip or transform
fault (example: the Dead Sea area).
Oceanic trench: a deep linear depression located in the ocean floor.
Oceanic trenches are caused by the subduction (when one tectonic
plate is pushed underneath another) of oceanic crust beneath either
other oceanic crust or continental crust.
Sedimentary related:
Sedimentary basin: In sedimentology, an area thickly filled with
sediment in which the weight of the sediment further depresses the
floor of the basin.
An anticyclone (that is, opposite to a cyclone) is
a weather phenomenon defined by the United States' National
Weather Service's glossary as large-scale circulation of winds
around a central region of high atmospheric pressure, clockwise in
the Northern Hemisphere, counterclockwise in the Southern
Hemisphere". Effects of surface-based anticyclones include
clearing skies as well as cooler, drier air. Fog can also form
overnight within a region of higher pressure. Mid- tropospheric
systems, such as the subtropical ridge, deflect tropical cyclones
around their periphery and cause a temperature
inversion inhibiting free convection near their center, building up
surface-based haze under their base. Anticyclones aloft can form
within warm core lows, such as tropical cyclones, due to
descending cool air from the backside of upper troughs, such as
polar highs, or from large scale sinking, such as the subtropical
ridge. Anticyclonic flow spirals in a clockwise direction in
the Northern Hemisphere and anticlockwise in the Southern
Hemisphere.
In the first investigations of Climate and Weather, your students
developed a working concept of air—a gas material that surrounds the
Earth, fills space and exerts pressure on its surroundings. In Weather 3,
you will help them to develop a concept of moving air or wind. Based on
observations of their surroundings and the behavior of a simple
instrument they make themselves, your students will learn to report two
properties of moving air; wind speed and direction.The idea that air
reaches us from different directions at different times may also be new to
young children. While they know wind occurs from time to time, they
may not notice the different wind directions. It is also unlikely that they
will associate different wind speeds and directions with particular
weather patterns. Do storms always come from the same direction? Do
high winds mean the weather is going to change? Do winds bring hot
weather or cold weather, or both? These are some of the questions that
young children may have never asked themselves because their focus in
on how the wind is acting on them at a given moment, not over long
periods of hours or days.
Weather and climate by Daniel Portelli 3.02
Weather and climate by Daniel Portelli 3.02
Weather and climate by Daniel Portelli 3.02

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Weather and climate by Daniel Portelli 3.02

  • 1.
  • 2.
  • 3. What Is the Difference Between Weather and Climate? It’s a sweltering midsummer day. “It must be global warming,” mutters someone. But is it the Earth’s changing climate that has made the day so warm? Or, is it just the weather that is so unbearable? Weather Weather is the mix of events that happen each day in our atmosphere including temperature, rainfall and humidity. Weather is not the same everywhere. Perhaps it is hot, dry and sunny today where you live, but in other parts of the world it is cloudy, raining or even snowing. Everyday, weather events are recorded and predicted by meteorologists worldwide. Climate Climate in your place on the globe controls the weather where you live. Climate is the average weather pattern in a place over many years. So, the climate of Antarctica is quite different than the climate of a tropical island. Hot summer days are quite typical of climates in many regions of the world, even without the affects of global warming.
  • 4.
  • 5.  The only type of severe  Called tornadoes over land weather event that we and waterspouts over ocean, these wild weather name individually, these events churn air at the are among Earth’s fastest speeds ever recorded largest and fiercest on Earth. While they are storms. Each storm is often short-lived, often only existing for a few able to, for a week or minutes, the intense winds more, travel thousands and flying debris from of miles stirring tornadoes can destroy seas, toppling everything in their path. trees, and leveling  buildings.  Hurricanes and typhoons Tornadoes and waterspouts
  • 6. These storms are common  Waking up in the morning in the spring and summer to find a fresh white when there is warm air near the ground and cool blanket of snow coating air above. Small the ground may be thunderstorms may only commonplace in many exist for an hour while areas, occurring several large Super cell storms can last for several hours times each winter, yet it spawning remains an exciting tornadoes, hail, intense surprise since predicting lightning, and flash winter storms is not easy. flooding.  Thunderstorms Blizzards
  • 7.
  • 8. Climate encompasses the statistics of, atmospheric pressure, wind, precipitation, atmospheric particle temperature, humidity count and other meteorological elemental measurements in a given region over long periods. Climate can be contrasted to weather, which is the present condition of these elements and their variations over shorter periods. A region's climate is generated by the climate system, which has five components: atmosphere, hydrosphere, cryosphere, land surface, and biosphere. The climate of a location is affected by its latitude, terrain, and altitude, as well as nearby water bodies and their currents. Climates can be classified according to the average and the typical ranges of different variables, most commonly temperature and precipitation. Paleo climatology is the study of ancient climates. Since direct observations of climate are not available before the 19th century, paleo climates are inferred from proxy variables that include non-biotic evidence such as sediments found in lake beds and ice cores, and biotic evidence such as tree rings and coral. Climate models are mathematical models of past, present and future climates. Climate change may occur over long and short timescales from a variety of factors; recent warming is discussed in global warming.
  • 9.
  • 10.
  • 11. A depression in geology is a landform sunken or depressed below the surrounding area. Depressions may be formed by various mechanisms. Structural or tectonic related: Structural basin: A circular, syncline-like depression; a region of tectonic down warping ( associated with a subduction zone and island arc); Graben or rift valley: down dropped and typically linear depressions or basin created by rifting in a region under tensional tectonic forces. Pull apart basin caused by offset in a strike slip or transform fault (example: the Dead Sea area). Oceanic trench: a deep linear depression located in the ocean floor. Oceanic trenches are caused by the subduction (when one tectonic plate is pushed underneath another) of oceanic crust beneath either other oceanic crust or continental crust. Sedimentary related: Sedimentary basin: In sedimentology, an area thickly filled with sediment in which the weight of the sediment further depresses the floor of the basin.
  • 12. An anticyclone (that is, opposite to a cyclone) is a weather phenomenon defined by the United States' National Weather Service's glossary as large-scale circulation of winds around a central region of high atmospheric pressure, clockwise in the Northern Hemisphere, counterclockwise in the Southern Hemisphere". Effects of surface-based anticyclones include clearing skies as well as cooler, drier air. Fog can also form overnight within a region of higher pressure. Mid- tropospheric systems, such as the subtropical ridge, deflect tropical cyclones around their periphery and cause a temperature inversion inhibiting free convection near their center, building up surface-based haze under their base. Anticyclones aloft can form within warm core lows, such as tropical cyclones, due to descending cool air from the backside of upper troughs, such as polar highs, or from large scale sinking, such as the subtropical ridge. Anticyclonic flow spirals in a clockwise direction in the Northern Hemisphere and anticlockwise in the Southern Hemisphere.
  • 13. In the first investigations of Climate and Weather, your students developed a working concept of air—a gas material that surrounds the Earth, fills space and exerts pressure on its surroundings. In Weather 3, you will help them to develop a concept of moving air or wind. Based on observations of their surroundings and the behavior of a simple instrument they make themselves, your students will learn to report two properties of moving air; wind speed and direction.The idea that air reaches us from different directions at different times may also be new to young children. While they know wind occurs from time to time, they may not notice the different wind directions. It is also unlikely that they will associate different wind speeds and directions with particular weather patterns. Do storms always come from the same direction? Do high winds mean the weather is going to change? Do winds bring hot weather or cold weather, or both? These are some of the questions that young children may have never asked themselves because their focus in on how the wind is acting on them at a given moment, not over long periods of hours or days.