The reason Marquette gets much more snow than Thunder Bay even though both Thunder Bay and Marquette are located on the shore of Lake Superior.

Question

Want to see more full solutions like this?

Answer 1

Question

Chapter 19, Problem 1GST

a)

To determine

The reason Marquette gets much more snow than Thunder Bay even though both Thunder Bay and Marquette are located on the shore of Lake Superior.

a)

Expert Solution

Answer to Problem 1GST

The reason Marquette receives more snow than Thunder Bay is because it is located on the leeward side of the Lake Superior, where continental polar air cools and falls as snow due to the condition known as Lake-effect snowfall.

Explanation of Solution

Lake-effect snow generally occurs in the late fall or early winter, when the dry continental polar air mass moves across a relatively warm Great Lakes waters. The air gains a great deal of heat and moisture by generating humid, unstable air that brings heavy snow to the land, over which the air mass moves next.

In the late autumn and early winter, the continental polar air from Canada blows across Lake Superior and picks up a considerable amount of moisture from the warmer lake waters. The saturated air cools when it hits the leeward shore, (where Marquette is located) and falls as snow in the areas around south and east of Lake Superior. Thunder Bay which is located on the windward shore received much lesser snow for this reason.

b)

To determine

The reason for the narrow, north-south zone of relatively heavy snow in the east of Pittsburgh and Charleston though the region is located too far from the Great Lakes to receive lake-effect snowfall and whether the reason explains the shape of this snowy zone.

b)

Expert Solution

Answer to Problem 1GST

The east of Pittsburgh and Charleston experiences heavy snow because of the orographic lifting of air along the Appalachian Mountains on the windward side of the slopes.

Explanation of Solution

As the maritime polar air arrives at the western shore of North America, it is often accompanied by low clouds and precipitation. When this air advances inland against the western mountains, the orographic lifting of air produces heavy rain or snow on the windward slopes of the mountains.

The band of heavy snow in the east of Pittsburgh and Charleston is caused by the lifting of air onto the higher Appalachian Mountains. The moist air rises and cools to the dew point as it is forced upward, resulting in an increased snowfall in the higher elevations.

Want to see more full solutions like this?

Subscribe now to access step-by-step solutions to millions of textbook problems written by subject matter experts!

Students have asked these similar questions

Title: Implementing low impact development: Sustainable water management solutions for urban areas Research questions: What are the economic, environmental, and social benefits of integrating wastewater recycling systems into urban water management practices? What methods can cities employ to resolve water supply needs with natural resource defense while achieving long-term water resource sustainability? Please answer all questions in the pictures in detail

18. 19. 20. - 15. 16. 17. The desired outcome of the curriculum delivered in environmental studies and sciences (ESS) programs at U.S. universities typically follow one of three ideal models- those focused on the systems sciences, those focused on policy and governance, or those focused on: a. adaptive management. b. environmental resource conservation. c. frontline practices of sustainability. Friedrich Ratzel's concept of lebensraum was turned to expansionist geopolitical ends through a particular reading of the work of Charles Darwin. One of the assumptions that Ratzel made in applying Darwin's ideas to the political world was that both animals and nation-states are: a. changing through the process of evolution. b. engaged in a competition where only the fittest will survive. c. surviving and developing in substantial part through cooperative strategies. In qualitative research, it often helps to distinguish between descriptive codes, which are often categorical or refer to simple…

30. 29. Climate scientist Mike Hulme argued that people who tend to see nature as benign or resilient, and who believe that we can adapt in part by making greener consumption choices and in part by embracing a future that will involve broadly tolerable levels of climate change, tend to be: a. egalitarians. b. hierarchists. c. individualists. Consider the following abstract from a research article published in a peer-reviewed journal titled Geographical Review: "Research on the human dimensions of global climate change should consider the way [that] at-risk populations confront uncertainty through cultural practices. This is a vital point for Indigenous peoples around the world, but particularly for those in the Arctic region where the effects of climate change are most dramatic. The Iñupiat of Arctic Alaska are especially susceptible to climatic and associated environmental changes, because they rely on sea ice to hunt the bowhead whale. [T]his paper reveals Iñupiaq cultural resilience…

Answer 2

Question

Chapter 19, Problem 1GST

a)

To determine

The reason Marquette gets much more snow than Thunder Bay even though both Thunder Bay and Marquette are located on the shore of Lake Superior.

a)

Expert Solution

Answer to Problem 1GST

The reason Marquette receives more snow than Thunder Bay is because it is located on the leeward side of the Lake Superior, where continental polar air cools and falls as snow due to the condition known as Lake-effect snowfall.

Explanation of Solution

Lake-effect snow generally occurs in the late fall or early winter, when the dry continental polar air mass moves across a relatively warm Great Lakes waters. The air gains a great deal of heat and moisture by generating humid, unstable air that brings heavy snow to the land, over which the air mass moves next.

In the late autumn and early winter, the continental polar air from Canada blows across Lake Superior and picks up a considerable amount of moisture from the warmer lake waters. The saturated air cools when it hits the leeward shore, (where Marquette is located) and falls as snow in the areas around south and east of Lake Superior. Thunder Bay which is located on the windward shore received much lesser snow for this reason.

b)

To determine

The reason for the narrow, north-south zone of relatively heavy snow in the east of Pittsburgh and Charleston though the region is located too far from the Great Lakes to receive lake-effect snowfall and whether the reason explains the shape of this snowy zone.

b)

Expert Solution

Answer to Problem 1GST

The east of Pittsburgh and Charleston experiences heavy snow because of the orographic lifting of air along the Appalachian Mountains on the windward side of the slopes.

Explanation of Solution

As the maritime polar air arrives at the western shore of North America, it is often accompanied by low clouds and precipitation. When this air advances inland against the western mountains, the orographic lifting of air produces heavy rain or snow on the windward slopes of the mountains.

The band of heavy snow in the east of Pittsburgh and Charleston is caused by the lifting of air onto the higher Appalachian Mountains. The moist air rises and cools to the dew point as it is forced upward, resulting in an increased snowfall in the higher elevations.

Want to see more full solutions like this?

Subscribe now to access step-by-step solutions to millions of textbook problems written by subject matter experts!

Answer 3

Question

Chapter 19, Problem 1GST

a)

To determine

The reason Marquette gets much more snow than Thunder Bay even though both Thunder Bay and Marquette are located on the shore of Lake Superior.

a)

Expert Solution

Answer to Problem 1GST

The reason Marquette receives more snow than Thunder Bay is because it is located on the leeward side of the Lake Superior, where continental polar air cools and falls as snow due to the condition known as Lake-effect snowfall.

Explanation of Solution

Lake-effect snow generally occurs in the late fall or early winter, when the dry continental polar air mass moves across a relatively warm Great Lakes waters. The air gains a great deal of heat and moisture by generating humid, unstable air that brings heavy snow to the land, over which the air mass moves next.

In the late autumn and early winter, the continental polar air from Canada blows across Lake Superior and picks up a considerable amount of moisture from the warmer lake waters. The saturated air cools when it hits the leeward shore, (where Marquette is located) and falls as snow in the areas around south and east of Lake Superior. Thunder Bay which is located on the windward shore received much lesser snow for this reason.

b)

To determine

The reason for the narrow, north-south zone of relatively heavy snow in the east of Pittsburgh and Charleston though the region is located too far from the Great Lakes to receive lake-effect snowfall and whether the reason explains the shape of this snowy zone.

b)

Expert Solution

Answer to Problem 1GST

The east of Pittsburgh and Charleston experiences heavy snow because of the orographic lifting of air along the Appalachian Mountains on the windward side of the slopes.

Explanation of Solution

As the maritime polar air arrives at the western shore of North America, it is often accompanied by low clouds and precipitation. When this air advances inland against the western mountains, the orographic lifting of air produces heavy rain or snow on the windward slopes of the mountains.

The band of heavy snow in the east of Pittsburgh and Charleston is caused by the lifting of air onto the higher Appalachian Mountains. The moist air rises and cools to the dew point as it is forced upward, resulting in an increased snowfall in the higher elevations.

Want to see more full solutions like this?

Subscribe now to access step-by-step solutions to millions of textbook problems written by subject matter experts!

Answer 4

Question

Chapter 19, Problem 1GST

a)

To determine

The reason Marquette gets much more snow than Thunder Bay even though both Thunder Bay and Marquette are located on the shore of Lake Superior.

a)

Expert Solution

Answer to Problem 1GST

The reason Marquette receives more snow than Thunder Bay is because it is located on the leeward side of the Lake Superior, where continental polar air cools and falls as snow due to the condition known as Lake-effect snowfall.

Explanation of Solution

Lake-effect snow generally occurs in the late fall or early winter, when the dry continental polar air mass moves across a relatively warm Great Lakes waters. The air gains a great deal of heat and moisture by generating humid, unstable air that brings heavy snow to the land, over which the air mass moves next.

In the late autumn and early winter, the continental polar air from Canada blows across Lake Superior and picks up a considerable amount of moisture from the warmer lake waters. The saturated air cools when it hits the leeward shore, (where Marquette is located) and falls as snow in the areas around south and east of Lake Superior. Thunder Bay which is located on the windward shore received much lesser snow for this reason.

b)

To determine

The reason for the narrow, north-south zone of relatively heavy snow in the east of Pittsburgh and Charleston though the region is located too far from the Great Lakes to receive lake-effect snowfall and whether the reason explains the shape of this snowy zone.

b)

Expert Solution

Answer to Problem 1GST

The east of Pittsburgh and Charleston experiences heavy snow because of the orographic lifting of air along the Appalachian Mountains on the windward side of the slopes.

Explanation of Solution

As the maritime polar air arrives at the western shore of North America, it is often accompanied by low clouds and precipitation. When this air advances inland against the western mountains, the orographic lifting of air produces heavy rain or snow on the windward slopes of the mountains.

The band of heavy snow in the east of Pittsburgh and Charleston is caused by the lifting of air onto the higher Appalachian Mountains. The moist air rises and cools to the dew point as it is forced upward, resulting in an increased snowfall in the higher elevations.

Want to see more full solutions like this?

Subscribe now to access step-by-step solutions to millions of textbook problems written by subject matter experts!

Answer 5

Chapter 19, Problem 1GST

a)

To determine

The reason Marquette gets much more snow than Thunder Bay even though both Thunder Bay and Marquette are located on the shore of Lake Superior.

a)

Expert Solution

Answer to Problem 1GST

The reason Marquette receives more snow than Thunder Bay is because it is located on the leeward side of the Lake Superior, where continental polar air cools and falls as snow due to the condition known as Lake-effect snowfall.

Explanation of Solution

Lake-effect snow generally occurs in the late fall or early winter, when the dry continental polar air mass moves across a relatively warm Great Lakes waters. The air gains a great deal of heat and moisture by generating humid, unstable air that brings heavy snow to the land, over which the air mass moves next.

In the late autumn and early winter, the continental polar air from Canada blows across Lake Superior and picks up a considerable amount of moisture from the warmer lake waters. The saturated air cools when it hits the leeward shore, (where Marquette is located) and falls as snow in the areas around south and east of Lake Superior. Thunder Bay which is located on the windward shore received much lesser snow for this reason.

b)

To determine

The reason for the narrow, north-south zone of relatively heavy snow in the east of Pittsburgh and Charleston though the region is located too far from the Great Lakes to receive lake-effect snowfall and whether the reason explains the shape of this snowy zone.

b)

Expert Solution

Answer to Problem 1GST

The east of Pittsburgh and Charleston experiences heavy snow because of the orographic lifting of air along the Appalachian Mountains on the windward side of the slopes.

Explanation of Solution

As the maritime polar air arrives at the western shore of North America, it is often accompanied by low clouds and precipitation. When this air advances inland against the western mountains, the orographic lifting of air produces heavy rain or snow on the windward slopes of the mountains.

The band of heavy snow in the east of Pittsburgh and Charleston is caused by the lifting of air onto the higher Appalachian Mountains. The moist air rises and cools to the dew point as it is forced upward, resulting in an increased snowfall in the higher elevations.

Answer 6

Chapter 19, Problem 1GST

a)

To determine

The reason Marquette gets much more snow than Thunder Bay even though both Thunder Bay and Marquette are located on the shore of Lake Superior.

a)

Expert Solution

Answer to Problem 1GST

The reason Marquette receives more snow than Thunder Bay is because it is located on the leeward side of the Lake Superior, where continental polar air cools and falls as snow due to the condition known as Lake-effect snowfall.

Explanation of Solution

Lake-effect snow generally occurs in the late fall or early winter, when the dry continental polar air mass moves across a relatively warm Great Lakes waters. The air gains a great deal of heat and moisture by generating humid, unstable air that brings heavy snow to the land, over which the air mass moves next.

In the late autumn and early winter, the continental polar air from Canada blows across Lake Superior and picks up a considerable amount of moisture from the warmer lake waters. The saturated air cools when it hits the leeward shore, (where Marquette is located) and falls as snow in the areas around south and east of Lake Superior. Thunder Bay which is located on the windward shore received much lesser snow for this reason.

Answer 7

Chapter 19, Problem 1GST

a)

To determine

The reason Marquette gets much more snow than Thunder Bay even though both Thunder Bay and Marquette are located on the shore of Lake Superior.

Answer 8

a)

Expert Solution

Answer to Problem 1GST

The reason Marquette receives more snow than Thunder Bay is because it is located on the leeward side of the Lake Superior, where continental polar air cools and falls as snow due to the condition known as Lake-effect snowfall.

Answer 9

a)

Expert Solution

Answer 10

a)

Expert Solution

Answer 11

Expert Solution

Answer 12

Explanation of Solution

Lake-effect snow generally occurs in the late fall or early winter, when the dry continental polar air mass moves across a relatively warm Great Lakes waters. The air gains a great deal of heat and moisture by generating humid, unstable air that brings heavy snow to the land, over which the air mass moves next.

In the late autumn and early winter, the continental polar air from Canada blows across Lake Superior and picks up a considerable amount of moisture from the warmer lake waters. The saturated air cools when it hits the leeward shore, (where Marquette is located) and falls as snow in the areas around south and east of Lake Superior. Thunder Bay which is located on the windward shore received much lesser snow for this reason.

Answer 13

b)

To determine

The reason for the narrow, north-south zone of relatively heavy snow in the east of Pittsburgh and Charleston though the region is located too far from the Great Lakes to receive lake-effect snowfall and whether the reason explains the shape of this snowy zone.

b)

Expert Solution

Answer to Problem 1GST

The east of Pittsburgh and Charleston experiences heavy snow because of the orographic lifting of air along the Appalachian Mountains on the windward side of the slopes.

Explanation of Solution

As the maritime polar air arrives at the western shore of North America, it is often accompanied by low clouds and precipitation. When this air advances inland against the western mountains, the orographic lifting of air produces heavy rain or snow on the windward slopes of the mountains.

The band of heavy snow in the east of Pittsburgh and Charleston is caused by the lifting of air onto the higher Appalachian Mountains. The moist air rises and cools to the dew point as it is forced upward, resulting in an increased snowfall in the higher elevations.

Answer 14

b)

To determine

The reason for the narrow, north-south zone of relatively heavy snow in the east of Pittsburgh and Charleston though the region is located too far from the Great Lakes to receive lake-effect snowfall and whether the reason explains the shape of this snowy zone.

Answer 15

b)

Expert Solution

Answer to Problem 1GST

The east of Pittsburgh and Charleston experiences heavy snow because of the orographic lifting of air along the Appalachian Mountains on the windward side of the slopes.

Answer 16

b)

Expert Solution

Answer 17

b)

Expert Solution

Answer 18

Expert Solution

Answer 19

Explanation of Solution

As the maritime polar air arrives at the western shore of North America, it is often accompanied by low clouds and precipitation. When this air advances inland against the western mountains, the orographic lifting of air produces heavy rain or snow on the windward slopes of the mountains.

The band of heavy snow in the east of Pittsburgh and Charleston is caused by the lifting of air onto the higher Appalachian Mountains. The moist air rises and cools to the dew point as it is forced upward, resulting in an increased snowfall in the higher elevations.