both are important precipitation -- rain and snow gages seasons are the result of the tilt of the Earth's axis -- the axis always points in the same direction, so different the two poles alternate pointing toward the Sun this causes changes in the day length, and consequently, the temperature cardinal days in the year are the vernal and autumnal equinoxes and the summer and winter solstices climate is the result of the geographic position higher latitudes have more seasonal variation, less warming latitude also influences the general pattern of wind and rain: equatorial doldrum, trade winds (from the east), horse latitudes with deserts (around 30-35 N and S), then the westerlies and polar easterlies;
(rain and snow gages seasons; are; the result of the tilt of the Earth's axis) (so different the two poles alternate pointing toward the Sun this causes changes in the day length; is; the result of the geographic position) (higher latitudes; have; more seasonal variation, less warming latitude also influences the general pattern of wind and rain) (the two poles; pointing; toward the Sun) (less warming latitude; also influences; the general pattern of wind and rain) (this; causes; changes in the day length, and consequently, the temperature cardinal days in the year are the vernal and autumnal equinoxes and the summer and winter solstices climate is the result of the geographic position higher latitudes have more seasonal variation, less warming latitude also influences the general pattern of wind and rain: equatorial doldrum, trade winds (from the east)
rain and snow gages seasons so different the two poles alternate pointing toward the Sun this causes changes in the day length higher latitudes the two poles less warming latitude this
are is have pointing also influences causes
the result of the tilt of the Earth's axis
the result of the geographic position
more seasonal variation, less warming latitude also influences the general pattern of wind and rain
toward the Sun
the general pattern of wind and rain
changes in the day length, and consequently, the temperature cardinal days in the year are the vernal and autumnal equinoxes and the summer and winter solstices climate is the result of the geographic position higher latitudes have more seasonal variation, less warming latitude also influences the general pattern of wind and rain: equatorial doldrum, trade winds (from the east