Land and Sea Breezes    

Land and sea breezes are caused by the difference in temperature between the land and the sea.   Land cools and heats quicker than water.  Thus, during the day the land is warmer than the water and during the night the land is cooler.  Since cooler air is heaver than warm, the colder air will flow toward and displace the warm air.  Thus, during the night and early morning as the land cools, a breeze will be felt traveling from land out to sea (land breeze) and during the afternoon, as the land warms, a breeze will be felt traveling from the sea to the land (sea breeze).   Sea breezes are stronger than land breezes and may obtain a strength of 10 to 15 knots.   The changing of the direction of the wind by 360 degrees in a 24 hour period will often cause a boat at anchor to swing around its entire anchor radius. 

Note:  Winds are described as where they blow from.  Currents are described as where they flow to.  Thus, a northerly wind blows from the north.  A northerly current flows toward the north.
      

Cold & Warm Fronts

Cold air is denser and than warm air and when pushed by weather systems forces a wedge under the warm air ahead of it. The denser air exerted higher pressure in the atmosphere reflected in a rising reading on a barometer. The reverse is true of warm air following a cold air mass. In each case the change in barometer indicate an instability which can cause bad weather conditions:  high winds, reduced visibility in fog or rain,  and lightening storms. A falling barometer often  means the approach of a weather front or deteriorating weather, as a rising barometer forecasts good weather.  The faster the barometer changes the more dramatic the weather.

Cold Front:  Cold air rapidly pushes beneath warm air.   This front can move fast, up to 25-30 knots, and weather deteriorates with rain, strong winds and thunderstorms.  
 
Warm Front:  Warm air slowly pushes over cold air.  This front moves slowly, 10 to 15 knots, and the weather slowly changes to showers.  However, this front can also bring strong winds and thunderstorms.
  
Stationary Front:  When warm and cold air of equal pressure are next to each other, no movement will take place.  Stationary fronts usually produce weather similar to a warm front but milder.
  

 
Clouds

Cirrus Clouds:   
 
Cirrus clouds or "Mare's tails" are thin wisps of high altitude clouds.  When followed by cirrostratus (high gauzy sheets) deteriorating weather may be approaching in 24 to 48 hours.
  










The picture to the right shows a few cirrus and cirrostratus clouds.
  
  

 
 
 
 
 
 

 
Cumulus Clouds: 
   
These are cauliflower like puffs of clouds.  If they  become taller they may produce thunderheads (cumulonimbus clouds).  If they stay the same height, fair weather can be predicted.
  
    
  
 
 
  
   
Thunderheads: 
  
Cumulonimbus clouds or thunderheads have anvil tops and produce high winds and storms.  The direction of the storm's travel is denoted by the anvil.

   
 
 



 
Storm Front: 
 
Rapidly moving black clouds mean the approaching of a storm.  The approach can be rapid with strong winds.  Sails should be rapidly reefed.