Feedback Loops and their Effect on The Climate System (No Local)

Front

What is a feedback loop in the climate system?

Back

A feedback loop is a process where the output of a system influences its own input, creating a cycle that can amplify or dampen changes in the system.

Front

What are the two types of feedback loops?

Back

Positive feedback loops amplify changes, while negative feedback loops counteract changes.

Front

How does a positive feedback loop affect climate change?

Back

A positive feedback loop can accelerate climate change, such as when melting ice reduces the Earth's albedo, leading to more heat absorption and further melting.

Front

What role does the Sun play in the climate system?

Back

The Sun provides the energy that drives the climate system, influencing temperature, weather patterns, and the water cycle.

Front

What is the water cycle?

Back

The water cycle is the continuous movement of water within the Earth and atmosphere, involving processes like evaporation, condensation, and precipitation.

Front

What happens during evaporation in the water cycle?

Back

During evaporation, water absorbs energy from the Sun and changes from liquid to vapor, which cools the surrounding environment.

Front

What is the definition of climate?

Back

Climate refers to the average weather conditions in a specific area over a long period, typically 30 years.

Front

How do marine west coast climates differ from Mediterranean climates?

Back

Marine west coast climates are characterized by mild temperatures and high precipitation, while Mediterranean climates have hot, dry summers and mild, wet winters.

Front

What is the significance of albedo in the climate system?

Back

Albedo is the measure of how much sunlight is reflected by a surface; surfaces with high albedo reflect more sunlight, influencing local and global temperatures.

Front

What is conduction in the context of heat transfer?

Back

Conduction is the transfer of heat through direct contact between materials, where heat moves from a warmer object to a cooler one.