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1.
MULTIPLE CHOICE QUESTION
1 min • 1 pt
Questions 1- 10
Precipitation, commonly referred to as rainfall, is a measure of the quantity of water in the form of either rain, hail, or snow which reaches the ground. The average annual precipi- tation over the whole of the United States is thirty-six inches. It should be understood however, that a foot of snow is not equal to a foot of precipitation. A general formula for
Line (5) computing the precipitation of snowfall is that ten inches of snow is equal to one inch of pre- cipitation. In New York State, for example, twenty inches of snow in one year would be recorded as only two inches of precipitation. Forty inches of rain would be recorded as forty inches of precipitation. The total annual precipitation would be recorded as forty-two inches. The amount of precipitation is a combined result of several factors, including location,
Line (10) altitude, proximity to the sea, and the direction of prevailing winds. Most of the precipitation in the United States is brought originally by prevailing winds from the Pacific Ocean, the Gulf of Mexico, the Atlantic Ocean, and the Great Lakes. Because these prevailing winds generally come from the West, the Pacific Coast receives more annual precipitation than the Atlantic Coast. Along the Pacific Coast itself, however, altitude causes some diversity in rain-
Line (15) fall. The mountain ranges of the United States, especially the Rocky Mountain Range and the Appalachian Mountain Range, influence the amount of precipitation in their areas. East of the Rocky Mountains, the annual precipitation decreases substantially from that west of the Rocky Mountains. The precipitation north of the Appalachian Mountains is about 40 percent
less than that south of the Appalachian Mountains.
What does this passage mainly discuss?
Precipitation
Snowfall
New York State
A general formula
2.
MULTIPLE CHOICE QUESTION
1 min • 1 pt
Questions 1- 10
Precipitation, commonly referred to as rainfall, is a measure of the quantity of water in the form of either rain, hail, or snow which reaches the ground. The average annual precipi- tation over the whole of the United States is thirty-six inches. It should be understood however, that a foot of snow is not equal to a foot of precipitation. A general formula for
Line (5) computing the precipitation of snowfall is that ten inches of snow is equal to one inch of pre- cipitation. In New York State, for example, twenty inches of snow in one year would be recorded as only two inches of precipitation. Forty inches of rain would be recorded as forty inches of precipitation. The total annual precipitation would be recorded as forty-two inches. The amount of precipitation is a combined result of several factors, including location,
Line (10) altitude, proximity to the sea, and the direction of prevailing winds. Most of the precipitation in the United States is brought originally by prevailing winds from the Pacific Ocean, the Gulf of Mexico, the Atlantic Ocean, and the Great Lakes. Because these prevailing winds generally come from the West, the Pacific Coast receives more annual precipitation than the Atlantic Coast. Along the Pacific Coast itself, however, altitude causes some diversity in rain-
Line (15) fall. The mountain ranges of the United States, especially the Rocky Mountain Range and the Appalachian Mountain Range, influence the amount of precipitation in their areas. East of the Rocky Mountains, the annual precipitation decreases substantially from that west of the Rocky Mountains. The precipitation north of the Appalachian Mountains is about 40 percent
less than that south of the Appalachian Mountains.
Which of the following is another word that is often used in place of precipitation?
Humidity
Wetness
Rainfall
Rain-snow
3.
MULTIPLE CHOICE QUESTION
1 min • 1 pt
Questions 1- 10
Precipitation, commonly referred to as rainfall, is a measure of the quantity of water in the form of either rain, hail, or snow which reaches the ground. The average annual precipi- tation over the whole of the United States is thirty-six inches. It should be understood however, that a foot of snow is not equal to a foot of precipitation. A general formula for
Line (5) computing the precipitation of snowfall is that ten inches of snow is equal to one inch of pre- cipitation. In New York State, for example, twenty inches of snow in one year would be recorded as only two inches of precipitation. Forty inches of rain would be recorded as forty inches of precipitation. The total annual precipitation would be recorded as forty-two inches. The amount of precipitation is a combined result of several factors, including location,
Line (10) altitude, proximity to the sea, and the direction of prevailing winds. Most of the precipitation in the United States is brought originally by prevailing winds from the Pacific Ocean, the Gulf of Mexico, the Atlantic Ocean, and the Great Lakes. Because these prevailing winds generally come from the West, the Pacific Coast receives more annual precipitation than the Atlantic Coast. Along the Pacific Coast itself, however, altitude causes some diversity in rain-
Line (15) fall. The mountain ranges of the United States, especially the Rocky Mountain Range and the Appalachian Mountain Range, influence the amount of precipitation in their areas. East of the Rocky Mountains, the annual precipitation decreases substantially from that west of the Rocky Mountains. The precipitation north of the Appalachian Mountains is about 40 percent
less than that south of the Appalachian Mountains.
The term precipitation includes
only rainfall
rain, hail, and snow
rain, snow, and humidity
rain, hail, and humidity
4.
MULTIPLE CHOICE QUESTION
1 min • 1 pt
Questions 1- 10
Precipitation, commonly referred to as rainfall, is a measure of the quantity of water in the form of either rain, hail, or snow which reaches the ground. The average annual precipi- tation over the whole of the United States is thirty-six inches. It should be understood however, that a foot of snow is not equal to a foot of precipitation. A general formula for
Line (5) computing the precipitation of snowfall is that ten inches of snow is equal to one inch of pre- cipitation. In New York State, for example, twenty inches of snow in one year would be recorded as only two inches of precipitation. Forty inches of rain would be recorded as forty inches of precipitation. The total annual precipitation would be recorded as forty-two inches. The amount of precipitation is a combined result of several factors, including location,
Line (10) altitude, proximity to the sea, and the direction of prevailing winds. Most of the precipitation in the United States is brought originally by prevailing winds from the Pacific Ocean, the Gulf of Mexico, the Atlantic Ocean, and the Great Lakes. Because these prevailing winds generally come from the West, the Pacific Coast receives more annual precipitation than the Atlantic Coast. Along the Pacific Coast itself, however, altitude causes some diversity in rain-
Line (15) fall. The mountain ranges of the United States, especially the Rocky Mountain Range and the Appalachian Mountain Range, influence the amount of precipitation in their areas. East of the Rocky Mountains, the annual precipitation decreases substantially from that west of the Rocky Mountains. The precipitation north of the Appalachian Mountains is about 40 percent
less than that south of the Appalachian Mountains.
What is the average annual rainfall in inches in the United States?
Thirty-six inches
Thirty-eight inches
Forty inches
Forty-two inches
5.
MULTIPLE CHOICE QUESTION
1 min • 1 pt
Questions 1- 10
Precipitation, commonly referred to as rainfall, is a measure of the quantity of water in the form of either rain, hail, or snow which reaches the ground. The average annual precipi- tation over the whole of the United States is thirty-six inches. It should be understood however, that a foot of snow is not equal to a foot of precipitation. A general formula for
Line (5) computing the precipitation of snowfall is that ten inches of snow is equal to one inch of pre- cipitation. In New York State, for example, twenty inches of snow in one year would be recorded as only two inches of precipitation. Forty inches of rain would be recorded as forty inches of precipitation. The total annual precipitation would be recorded as forty-two inches. The amount of precipitation is a combined result of several factors, including location,
Line (10) altitude, proximity to the sea, and the direction of prevailing winds. Most of the precipitation in the United States is brought originally by prevailing winds from the Pacific Ocean, the Gulf of Mexico, the Atlantic Ocean, and the Great Lakes. Because these prevailing winds generally come from the West, the Pacific Coast receives more annual precipitation than the Atlantic Coast. Along the Pacific Coast itself, however, altitude causes some diversity in rain-
Line (15) fall. The mountain ranges of the United States, especially the Rocky Mountain Range and the Appalachian Mountain Range, influence the amount of precipitation in their areas. East of the Rocky Mountains, the annual precipitation decreases substantially from that west of the Rocky Mountains. The precipitation north of the Appalachian Mountains is about 40 percent
less than that south of the Appalachian Mountains.
If a state has 40 inches of snow in a year, by how much does this increase the annual precipitation?
By two feet
By four inches
By four feet
By 40 inches
6.
MULTIPLE CHOICE QUESTION
1 min • 1 pt
Questions 1- 10
Precipitation, commonly referred to as rainfall, is a measure of the quantity of water in the form of either rain, hail, or snow which reaches the ground. The average annual precipi- tation over the whole of the United States is thirty-six inches. It should be understood however, that a foot of snow is not equal to a foot of precipitation. A general formula for
Line (5) computing the precipitation of snowfall is that ten inches of snow is equal to one inch of pre- cipitation. In New York State, for example, twenty inches of snow in one year would be recorded as only two inches of precipitation. Forty inches of rain would be recorded as forty inches of precipitation. The total annual precipitation would be recorded as forty-two inches. The amount of precipitation is a combined result of several factors, including location,
Line (10) altitude, proximity to the sea, and the direction of prevailing winds. Most of the precipitation in the United States is brought originally by prevailing winds from the Pacific Ocean, the Gulf of Mexico, the Atlantic Ocean, and the Great Lakes. Because these prevailing winds generally come from the West, the Pacific Coast receives more annual precipitation than the Atlantic Coast. Along the Pacific Coast itself, however, altitude causes some diversity in rain-
Line (15) fall. The mountain ranges of the United States, especially the Rocky Mountain Range and the Appalachian Mountain Range, influence the amount of precipitation in their areas. East of the Rocky Mountains, the annual precipitation decreases substantially from that west of the Rocky Mountains. The precipitation north of the Appalachian Mountains is about 40 percent
less than that south of the Appalachian Mountains.
The phrase "proximity to" in line 10 is closest in meaning to
communication with
dependence on
nearness to
similarity to
7.
MULTIPLE CHOICE QUESTION
1 min • 1 pt
Questions 1- 10
Precipitation, commonly referred to as rainfall, is a measure of the quantity of water in the form of either rain, hail, or snow which reaches the ground. The average annual precipi- tation over the whole of the United States is thirty-six inches. It should be understood however, that a foot of snow is not equal to a foot of precipitation. A general formula for
Line (5) computing the precipitation of snowfall is that ten inches of snow is equal to one inch of pre- cipitation. In New York State, for example, twenty inches of snow in one year would be recorded as only two inches of precipitation. Forty inches of rain would be recorded as forty inches of precipitation. The total annual precipitation would be recorded as forty-two inches. The amount of precipitation is a combined result of several factors, including location,
Line (10) altitude, proximity to the sea, and the direction of prevailing winds. Most of the precipitation in the United States is brought originally by prevailing winds from the Pacific Ocean, the Gulf of Mexico, the Atlantic Ocean, and the Great Lakes. Because these prevailing winds generally come from the West, the Pacific Coast receives more annual precipitation than the Atlantic Coast. Along the Pacific Coast itself, however, altitude causes some diversity in rain-
Line (15) fall. The mountain ranges of the United States, especially the Rocky Mountain Range and the Appalachian Mountain Range, influence the amount of precipitation in their areas. East of the Rocky Mountains, the annual precipitation decreases substantially from that west of the Rocky Mountains. The precipitation north of the Appalachian Mountains is about 40 percent
less than that south of the Appalachian Mountains.
Where is the annual precipitation highest?
The Atlantic Coast
The Great Lakes
The Gulf of Mexico
The Pacific Coast
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