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more about mountain weather


  WEATHER FACTS

WIND
wind

  • wind = air moving from high to low pressure
  • is invisible / seen by it's effect on other things
  • moves around / over/ forced through obstacles
  • at fast speeds wind currents similar to white water
  • hence wind-tunnels, eddies, sudden surges etc
  • go to Beaufort Wind Scale

TEMPERATURE
temperature thermometer

  • Drops by 1-2°C per 200m of ascent in altitude
  • Mountain summits are colder than valley floors
  • Rarely there can be a temperature inversion
  • Temperatures can drop suddenly
  • Extremes of heat carry danger

WIND-CHILL EFFECT


wind chill effect

  • Wind Chill lowers the temperature more

wind chill factor

  • Loss in °C = approx 1/2 x Wind Speed

wind chill chart

RAINFALL
raindrop

  • Rain drops can fall at speeds of ≤ 22 mph
  • Rain starts off as ice or snow crystals at cloud level
  • Light rain = ≤ 0.1" Heavy rain = ≥ 0.3" inches per hour
  • Rain drops size = 0.02 to 0.031 inches
  • Rain is recycled water that evaporated from our world's lakes, rivers, oceans, seas, waters

MIST / FOG
mountain mist

  • Mist = mass of fine droplets of water in the atmosphere near or in contact with the earth
  • density and wetness varies
  • Dense Mist = Fog obscuring visibiliy further
  • visibilitiy varies and can be as little as 5m

SNOW
snow + ice

  • snow = made up of ≥ 200 frozen ice crystals
  • crystals are 6-sided, all unique in size & shape
  • snow forms clouds where temperature < freezing
  • texture of snow varies: soft to hard, binding or loose

ICE
snow + ice

  • water freezes to become ice at 0°C (32°F)
  • ice varies in thickness from a thin sheet to inches
  • a lake's surface is the first bit to freeze

ELECTRICAL STORMS
lightning charge

  • Thunder clouds can build up static charge
  • Lightning = atmospheric discharge of electricity
  • Bolt can travel at 60,000 m/s (220,000 km/h)
  • Lightning temperature = ≤ 30,000°C (54,000°F)
  • Thunder = sonic shock wave made by lightning
  • Time-lag of flash to thunder = distance of storm
  • 2.9 secs time-lag = 1 km distance away


WEB-CAMS | CALENDAR WALKS 2010 | BOOKINGS



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