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A radar image from Springfield, Missouri is shown below. Three points are each marked with a bold X. Point 3 is the location of the radar. Points 1 and 2 are 120 and 60 miles west of the radar location, respectively. (a) At which point is the precipitation the heaviest 1 / 2 / 3  (b) The elevation angle of this radar scan is 0.5∘. At which point is the radar beam the highest?  1 / 2 / 3

A radar image from Springfield, Missouri is shown below. Three points are each marked with a bold X. Point 3 is the location of the radar. Points 1 and 2 are 120 and 60 miles west of the radar location, respectively. (a) At which point is the precipitation the heaviest 1 / 2 / 3  (b) The elevation angle of this radar scan is 0.5∘. At which point is the radar beam the highest?  1 / 2 / 3

Applications and Investigations in Earth Science (9th Edition)
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
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A radar image from Springfield, Missouri is shown below. Three points are each marked with a bold X. Point 3 is the location of the radar. Points 1 and 2 are 120 and 60 miles west of the radar location, respectively.

(a) At which point is the precipitation the heaviest

1 / 2 / 3 

(b) The elevation angle of this radar scan is 0.5∘. At which point is the radar beam the highest? 

1 / 2 / 3 

The image is a weather radar map showing a color-coded reflectivity scale typically used to identify precipitation intensity. The map is likely from a specific region, segmented by state borders. ### Color Scale: - **Light Blue (0-5 dBZ)**: Represents very light precipitation or no precipitation. - **Green (10-30 dBZ)**: Indicates light to moderate rain. - **Yellow (40-50 dBZ)**: Signifies heavier rain. - **Orange/Red (55-70 dBZ)**: Denotes intense rainfall, which may be associated with thunderstorms. - **Pink/Purple (75 dBZ and above)**: Extremely heavy precipitation, often linked to severe weather like hail. ### Analysis: - The radar map displays a significant band of heavy to severe precipitation running from the southwest to northeast. - The most intense weather, indicated by red and orange colors, is located in a central vertical band. - Three black Xs are present on the map, marked as 1, 2, and 3, suggesting specific points of interest or measurement locations. ### Date and Time: - The map is dated Tuesday, November 10, 1998, at 00:00 UTC. This type of radar imagery is important for meteorologists to interpret weather conditions, track storm systems, and issue warnings for severe weather events.
Transcribed Image Text:The image is a weather radar map showing a color-coded reflectivity scale typically used to identify precipitation intensity. The map is likely from a specific region, segmented by state borders. ### Color Scale: - **Light Blue (0-5 dBZ)**: Represents very light precipitation or no precipitation. - **Green (10-30 dBZ)**: Indicates light to moderate rain. - **Yellow (40-50 dBZ)**: Signifies heavier rain. - **Orange/Red (55-70 dBZ)**: Denotes intense rainfall, which may be associated with thunderstorms. - **Pink/Purple (75 dBZ and above)**: Extremely heavy precipitation, often linked to severe weather like hail. ### Analysis: - The radar map displays a significant band of heavy to severe precipitation running from the southwest to northeast. - The most intense weather, indicated by red and orange colors, is located in a central vertical band. - Three black Xs are present on the map, marked as 1, 2, and 3, suggesting specific points of interest or measurement locations. ### Date and Time: - The map is dated Tuesday, November 10, 1998, at 00:00 UTC. This type of radar imagery is important for meteorologists to interpret weather conditions, track storm systems, and issue warnings for severe weather events.
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