land and sea breezes are alike because they are both convection currents.
They are both convection currents
as the both are breezes i-e cool air.
When it's in the day, the land heats up faster than the water in the sea, so hot air rises from the land and cold air from the sea takes its place. So this results in sea breeze.
ocean currents & land- sea breeze.
Two forms of heat transfer help create a sea breeze are conduction and convection. Another form of heat transfer help create a sea breeze is radiation.
During the daytime the land warms relative to the cooler ocean or lake waters. If the atmosphere is vertically unstable the warm air being less dense than the surrounding air and lifts until condensation forms. A line of clouds and eventually showers and possibly thunderstorms develops. This warming also cause low pressure (by the gas formula) over land and air is pulled in from the ocean or lake. This is called a sea or lake breeze front. Out over the cooler waters the pressure is higher relative to the land and the air sinks and is pushed toward the land and a small scale circulation develops.After sundown the reverse physical processes occur and the land becomes relatively cooler than the lake or ocean water sometimes and a small scale circulation called a land breeze develops. These are not typically as strong as the sea breeze circulations and less evidence is seen in the form of clouds and showers.The sea breeze front shows up very nicely in the summertime, especially in Florida and across Cuba. Check your search engine with Sea Breeze front on GOES satellite imagery.
During the daytime the land warms relative to the cooler ocean or lake waters. If the atmosphere is vertically unstable the warm air being less dense than the surrounding air and lifts until condensation forms. A line of clouds and eventually showers and possibly thunderstorms develops. This warming also cause low pressure (by the gas formula) over land and air is pulled in from the ocean or lake. This is called a sea or lake breeze front. Out over the cooler waters the pressure is higher relative to the land and the air sinks and is pushed toward the land and a small scale circulation develops.After sundown the reverse physical processes occur and the land becomes relatively cooler than the lake or ocean water sometimes and a small scale circulation called a land breeze develops. These are not typically as strong as the sea breeze circulations and less evidence is seen in the form of clouds and showers.The sea breeze front shows up very nicely in the summertime, especially in Florida and across Cuba. Check your search engine with Sea Breeze front on GOES satellite imagery.
A sea breeze. A land breeze blows from land to sea.
Land breeze is in the air sea breeze is in the water
It is typically a very strong sea breeze, accompanied by very heavy rains.
sea breeze
land and sea breeze are each others opposites
A land breeze is wind that originates from the clashing of winds on land (tornado), and sea breeze originates from the sea.
Land breezes and sea breezes are both breeze, or cool air.
A sea breeze is a wind that blows from the sea towards the land.
The only difference - is the direction of flow. A sea breeze blows from the sea onto the land. A land breeze flows in the opposite direction.
It is called a land breeze
land breeze
land breeze sea breeze