Physical Geography Lab Exam 1

Graphic scale

The use of a line marked off in graduated distances as a map scale.

Fractional scale

-Representative fraction describing the ratio b/w distance on the map and the actual distance on earth's surface it represents.
-assumes that the same units of measurement (e.g. 1map in=200,000 earth in

Large-scale map

A map with a scale that is relatively large representative fraction and therefore portrays only a small portion of the earths surface.

Small-scale map

A map whose scale is a relatively small representative fraction and therefore shows a large portion of earths surface in limited detail

Isoline

A line on a map connecting points that have the same quality or intensity of a given phenomenon.

Contour line

a line joining two points of equal elevation

Contour interval

The difference in elevation between two elevation contour lines.

Depression contour

Elevation contour line with hachure marks pointing downslope into a depression

Relief

The difference in elevation between the highest and lowest points in an area; the vertical variation from mountain top to valley bottom.

Index contour

Every fourth or fifth contour line on most contour line maps; thicker than regular contour lines; usually marked with elevation.

Isotherm

A line on a map joining points of equal temperature.

Isobar

A line on a map joining points of equal atmospheric pressure.

Insolation

incoming solar raidation

Angle of incidence

The angle at which the sun's rays strike the earths surface.

Station model

Standardized system of data presentation used on a weather map to convey conditions at a weather station.

Friction

The force that impedes the relative motion of two objects in contact

Coriolis effect

The apparent deflection of free moving objects to the right in the northern hemisphere and to the left in the southern hemisphere, in response to the rotation of the earth

Humidity

Water vapor in the air

Mixing ratio

Description of the water vapor content of the air expressed as the mass of water in a given mass of dry air; usually as grams of water vapor per kilogram of dry air.

Saturation mixing ratio (SMR)

The water vapor capacity of air at a given temperature.

Saturation

Circumstances in which the air contains the maximum amount of water vapor for a given temperature;

Relative humidity

MR/SMR; an expression of the amount of water vapor in the air in comparison with the total amount there could be if the air were saturated. This ratio is expressed as a percentage.

Dew point

The critical air temperature at which water vapor saturation is reached.

Warm front

The leading edge of an advancing warm air mass

Cold front

The leading edge of an advancing cool air mass actively displacing warm air.

The 5 factors that control temperature

1. Latitude
2. Land-and-Water Contrast
3. Ocean Currents
4. Wind Patterns
5. Altitude

The 3 factors that affect daily insolation

1. Angle of Incidence
2. Length of Day
3. Atmospheric Obstruction.

Temperature change with altitude change

In general, temperature decreases with increased altitude.

Rate of temperature change (average lapse rate)

3.6�F per 1000 ft
6.5�C per 1000 m

Descending air in terms of pressure

Produces High Pressure near the earths surface

Ascending air in terms of pressure

Produces low pressure near the earths surface

Wind direction in upper atmosphere

In the northern hemisphere, the air encounters little friction. The balance of the pressure gradient force and the Coriolis effect result in winds that blow parallel to isobars (geostrophic winds), clockwise around highs, and counterclockwise around lows.

Wind direction at the surface

In the northern hemisphere, Friction is increased so the Coriolis effect deflection is reduced. Near the surface, the balance of the pressure gradient force, Coriolis effect, and friction results in winds that diverge clockwise out of highs (anticyclones)

Air movement around low pressure systems

In the northern hemisphere, air moves in a counter clockwise direction.

Air movement around high pressure systems

In the northern hemisphere, air moves in a clockwise direction.

Relationship among temperature, SMR, mixing ratio, dew point, and relative humidity

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