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Unit 4 Weather and Climate

Unit 4 Weather and Climate

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Unit 4 Weather and Climate

What  is  the  difference  between  ‘weather’  and  ‘climate’?    

     Weather:  The  state  of  the  atmosphere  at  a  given  <me  and  place,  with  respect  to  variables  such  as  Temp,  Moisture,  Wind  Air  pressure        

Copyright  ©  2010  Ryan  P.  Murphy  

Climate:  The  average  weather  of  a  par<cular  part  of  the  world  at  different  <mes  of  the  year.  

Copyright  ©  2010  Ryan  P.  Murphy  

Weather and Climate are Related

Where is this?

Camping  on  deposi<onal  sand  bars    

Petroglyphs  are  carvings  that  are  incised,  abraded  or  ground  by  means  of  stone  tools  upon  cliff  walls,  boulders  and  flat  bedrock  

surfaces.  

Can you spot the wildlife?

HI Capacity or high Competence?

What  helps  explains  the  transi<on  from  interior  dry-­‐lands  to  coastal  

rainforest?    

 Mountains,  “Rain-­‐shadows”  and  “Orographic”  Rainfall  

World Climate Zones

Tropical Climates Tropical moist climates extend north and south from the equator to about 15° to 25° latitude. In these climates all months have average temperatures greater than 64°F (18°C) and annual precipitation greater than 59".

Dry Climates Loss of water exceeds precipitation. These climates extend from 20°-35° North and South of the equator and in large continental regions of the mid-latitudes often surrounded by mountains.

Arid Environments

Evaporation is the process by which water changes from a liquid to a gas or vapor. Transpiration evaporation of water through minute pores, or stomata, in the leaves of plants.

Semi Arid Environments

Temperate. In this zone, there are typically warm and humid summers with thunderstorms and mild winters.

Continental. These regions have warm to cool summers and very cold winters. In the winter, this zone can experience snowstorms, strong winds, and very cold temperatures—sometimes falling below -22°F (-30°C)!

Polar Climates Polar climates have year-round cold temperatures with the warmest month less than 50°F (10°C). Polar climates are found on the northern coastal areas of North America, Europe, Asia, and on the land masses of Greenland and Antarctica.

What  factors  affect  weather  and  climate?    

(1) Atmosphere  –  our  focus  for  today,  however…      (2) The  Water  Cycle      (3) The  Sun    (4) The  Ocean    

(1)  The  Atmosphere:  A  star<ng  point  –  comes  from  Greek  “atmos”  meaning  vapour  and  “Sphairia”  meaning  ball    

Our  atmosphere  is  composed  of  78%  nitrogen  and  21%  oxygen;  the  rest  is  made  up  of  small  amounts  

of  trace  gases.    

•  This  thin  layer  is  our  atmosphere.  

Importance  of  the  atmosphere….  

Copyright  ©  2010  Ryan  P.  Murphy  

1.  Keeps  planet  warm  –  via  the  Greenhouse  Effect  –    

   -­‐  Heat  is  trapped  close  to  the  surface  of  the  Earth  by  “greenhouse  gases  ”  carbon  dioxide,  methane  and  nitrous  oxides.      -­‐  Like  a  blanket  wrapped  around  the  Earth,  which  keeps  it  toas<er  than  it  would  be  without  them.    

Copyright  ©  2010  Ryan  P.  Murphy  

Greenhouse  effect  also  means  we  find  water  in  all  three  states..    

Copyright  ©  2010  Ryan  P.  Murphy  

•  The  Moon  does  not  have  an  atmosphere  and  is  extremely  cold  in  the  shade,  and  extremely  hot  in  the  sun.  

     2.  Provides  oxygen  to  breathe  

Copyright  ©  2010  Ryan  P.  Murphy  

3.  Protects  us  from  small  meteors.  

Copyright  ©  2010  Ryan  P.  Murphy  

•  4.  Has  ozone  that  protects  us  from  radia<on  (UV).  

Copyright  ©  2010  Ryan  P.  Murphy  

•  Title:  Layers  of  the  Atmosphere  

 Layers  determined  by  temperature  

Troposphere  •  Weather  occurs  here    •  Life  occurs  here  •  0-­‐12  Km  

Stratosphere    Located  above  the  troposphere  and  below  the  mesosphere:  12-­‐50  km    -­‐  Air  planes  fly  here  •  Contains  “good  ozone”  layer  •  The  ozone  layer  helps  protect  us  from  ultraviolet  radia<on  (UV)  from  the  sun  

Mesosphere  •  The  mesosphere  starts  just  above  the  stratosphere  and  extends  to  85  kilometers  (53  miles)  high.  Meteors  burn  up  in  this  layer  

Thermosphere  •  The  thermosphere  starts  just  above  the  mesosphere  and  extends  to  600  kilometers  (372  miles)  high.  Aurora  and  satellites  occur  in  this  layer.  

Exosphere  •  This  is  the  upper  limit  of  our  atmosphere.  It  extends  from  the  top  of  the  thermosphere  up  to  10,000  km  (6,200  mi).  

Atmospheric  pollu<on  

Air  Pollu<on  can  be….    

Global

a)Global  Warming  =  Climate  Change  

•  hips://www.youtube.com/watch?v=oJAbATJCugs  

b)  Ozone  Deple<on    Ozone  is  important!    •  absorbs  most  of  the  UV  radia<on  from  sun.    •  Life  as  we  know  it  wouldn’t  be  possible  without  this  layer  of  protec<on.  

•  hips://ozonewatch.gsfc.nasa.gov/ozone_maps/movies/OZONE_D1979-­‐11%25P1Y_G%5e1920X1080.IOMPS_PNPP_V21_MMERRA2_LSH.mp4  

•  Thinning  rather  than  an  “hole”  •  The  regula<on  of  chemicals  has  helped  

•  hips://www.youtube.com/watch?v=aU6pxSNDPhs&t=7s  

Depletion of the Ozone layer vs Climate Change These two issues can become very confused in some people’s minds.

Depletion of ozone layer (ozone hole) •  The ozone layer is in the stratosphere. •  This ozone is created when high-energy

UV strikes an oxygen molecule – a natural process.

•  Ozone protects us from UV radiation •  Depletion of ozone (the ozone hole) was

caused by long-living chemicals, CFCs, that humans released into the atmosphere.

•  International agreements such as the Montreal Protocol have banned the use of CFCs.

•  There is a good chance that the ozone hole will mend in the near future

•  This is a relatively straightforward issue

Climate Change (CC) or Global warming •  Greenhouse gases (GHG) e.g. CO2 are found in

the troposphere. •  GHGs are important for keeping Earth warm

because they form an invisible layer that traps heat that is radiating away from Earth.

•  But extra GHGs are accumulating in the atmosphere because of human activity.

•  So extra heat is being trapped, warming the surface of the Earth.

•  The climate system is affected by many factors which makes the issue very complex e.g. the Earth is warming but some parts are getting colder

•  CC can not be easily fixed.

Climate  Change  and  Ozone  Deple<on  

•  Read  the  webpage  on  Ozone  Deple<on  and  Climate  Change  and  answer  the  ques<ons  posted  to  our  website.    

•  hips://www.canada.ca/en/environment-­‐climate-­‐change/services/air-­‐pollu<on/issues/ozone-­‐layer/deple<on-­‐climate-­‐change.html  

•  hips://www.youtube.com/watch?v=08z_xW-­‐szwM    

Focus  Ques<on    •  Climate  change  is  a  complex  problem.  But  we’ve  successfully  

addressed  environmental  problems  before.  Ozone  deple<on  is  an  example.  When  watching  the  video  think  about  this:    

•  What  can  we  learn  from  the  story  of  ozone  deple<on  that  might  help  to  address  climate  change?  

•  Write  down  some  ideas  from  the  video.    

•  hips://www.youtube.com/watch?v=08z_xW-­‐szwM    

Regional  Air  Pollu<on:  Acid  rain    •  hips://www.youtube.com/watch?v=1PDjVDIrFec&t=4s    

Regional – read and explain to your partner….

Acid rain -results when sulfur dioxide (SO2) and nitrogen oxides (NOX) are emitted into the atmosphere and transported by wind and air currents. SO2 and NOX react with water, oxygen and other chemicals to form sulfuric and nitric acids. These mix with water and other materials before falling to the ground Major sources of SO2 and NOX in the atmosphere are: 1) Burning of fossil fuels to generate electricity. Two thirds of SO2 and one fourth of NOX in the atmosphere come from electric power generators. 2) Vehicles and heavy equipment. 3) Manufacturing, oil refineries and other industries. Winds can blow SO2 and NOX over long distances and across borders making acid rain a problem for everyone and not just those who live close to these sources. .

Local  Air  Pollu<on:  Smog  and  Urban  Heat  Islands  

Smog over Shanghai Towers, China

Smog, Los Angles

Smog, Cairo

https://www.youtube.com/watch?v=CdbBwIgq4rs

Lets  take  a  test….    

•  hips://ed.ted.com/lessons/the-­‐science-­‐of-­‐smog-­‐kim-­‐preshoff/review_open#ques<on-­‐1  

Smog is ground level ozone – or bad ozone.

Produced when sunlight reacts with nitrogen oxides and at least one volatile organic compound (VOC) in the atmosphere. Nitrogen oxides come from car exhaust, coal power plants, and factory emissions. VOCs are released from gasoline, paints, and many cleaning solvents. When sunlight hits these chemicals, they form airborne particles and ground-level ozone—or smog.

Reducing  Smog:  What  can  you  do?      •  Drive  less.      •  Take  care  of  cars.  Gezng  regular  tune-­‐ups,  changing  oil  on  schedule,  and  

infla<ng  <res  to  the  proper  level  can  improve  gas  mileage  and  reduce  emissions.  

•  Fuel  up  during  the  cooler  hours  of  the  day—night  or  early  morning.  This  prevents  gas  fumes  from  hea<ng  up  and  producing  ozone.  

•  Avoid  products  that  release  high  levels  of  VOCs.  For  example,  use  low-­‐VOC  paints.  

•  Avoid  gas-­‐powered  yard  equipment,  like  lawn  mowers.  Use  electric  appliances.  Or  use  people  powered  tools  instead.    

Urban Heat Islands

Reading about urban heat islands - https://www.nationalgeographic.org/encyclopedia/urban-heat-island/ 1) What is an urban heat island? 2) What causes an urban heat island to develop? 3) How do urban heat islands affect air quality? 4) How do urban heat islands affect water quality? 5) How do urban heat islands contribute to global warming? 6) What can be done to reduce the effects of urban heat islands? 4

Urban Heat Islands

Urban  Forest  Strategy  •  Vancouver  on  track  to  plant  150,000  trees  by  the  year  2020:  126,000  so  far.  

•  Also  working  on  plan<ng  in  areas  with  rela<vely  liile  tree  cover    

Recap  –  what  we  learned      •  Weather  and  climate    

–  How  they  are  related  but  different  concepts  –  Local  example  –  wet  west  coast  vs.  dry  interior    –  5  World  Climate  Zones  –  The  atmosphere  –  its  importance  and  layers  –  Atmosphere  pollu<on  –  Global,  Regional  Local  examples