Physical Geography: Introduction to Weather, Climate, and Atmospheric Structure
Contextual Information and Chapter Identification
- Reference Page: 67
- Unit Segment: Settlements I
- Fragmentary Section Context: "ristics of nd Urban lements- ship arce"
- Main Subject Heading: 89 PHYSICAL GEOGRAPHY
- Chapter Title: Chapter-1 WEATHER AND CLIMATE
1.1 Introduction to the Atmosphere
- Central Relationship: Any discussion regarding weather and climate necessitates a focus on the atmosphere. This is because the atmosphere is the environment where the creation and subsequent changes of weather and climate occur.
- The Presence of Air: Air surrounds the earth and its inhabitants in all directions.
- Physical Perception: Although air is invisible to the human eye, it is described as being everywhere, and humans are characterized as "sinking in air."
Definition and Physical Properties of the Atmosphere
- Verbatim Definition: The gaseous layer of air that extends upward from the earth's surface and surrounds the earth is called the atmosphere.
- Atmospheric Attachment: The layer of air is held to the surface of the earth by the earth's gravitational force.
- Vertical Dimensions: The atmosphere is estimated to extend roughly to a height of approximately 10,000km from the surface of the earth.
Classification of Atmospheric Layers
- Structural Divisions: The atmosphere is categorized into four distinct layers:
- Troposphere
- Stratosphere
- Mesophere (Note: Verbatim spelling from the source text)
- Thermosphere
Characteristics and Meteorological Significance of the Troposphere
- Positional Status: The Troposphere is identified as the lowest layer of the atmosphere.
- Surface Proximity: It is the layer most closely attached to the earth's surface.
- Moisture Profile: This layer contains high levels of moisture.
- Meteorological Activity: Because of its close contact with the surface and its moisture content, the Troposphere is the site where all weather phenomena occur.
- Specific Weather Processes: The creation of clouds and the occurrence of rainfall take place specifically within the Troposphere.