produce stratus type clouds.
Upslope fog
Foehn winds, also called chinook winds east of the Rocky Mountains, and Santa Ana winds in southern California.
In general, it does not, though it varies by region. Much of Canada is relatively dry, especially in the central and north regions, so not a lot of snow falls despite being so snow. For example, a lot of snow falls in the US Rockies because of the upslope effect of the mountains, so comparing this to the Canadian Plains would be kind of unfair.
Texas has 2 Time Zones: Mountain Time Texas: Daylight Saving Time: This time is 6 time zones to England Standard Time: This time is 7 time zones to England Central Time Texas: Daylight Saving Time: 5 Time Zones Standard Time: 6 Time Zones
Upslope fog forms when air moves gently up in elevation enough for the layer to reach saturation.
An upslope fog is a fog created when moist air is lifted by a mountain or an upward sloping terrain. Condensation then occurs near the ground to form clouds.
upslope fog
radiation fog
produce stratus type clouds.
Upslope fog
Upslope fog
Upslope is the only possibility because it's the only one where the air is rising.
An anabatic wind is an upslope wind - when the wind is blowing up a hill or mountain as a result of local surface heating.
look in ch. 31 of your textbook
Within the city of Hilo, average rainfall varies from about 130 inches a year near the shore to as much as 200 inches upslope
Foehn winds, also called chinook winds east of the Rocky Mountains, and Santa Ana winds in southern California.