Question
If the specific heat capacity of water were smaller than it is, how would this affect oceans and climate?(1 point)
Responses
The oceans could absorb less heat, leading to a more steady temperature on land.
The oceans could absorb less heat, leading to a more steady temperature on land.
The oceans could absorb more heat, leading to greater swings in temperature on land.
The oceans could absorb more heat, leading to greater swings in temperature on land.
The oceans could absorb more heat, leading to a more steady temperature on land.
The oceans could absorb more heat, leading to a more steady temperature on land.
The oceans could absorb less heat, leading to greater swings in temperature on land.
The oceans could absorb less heat, leading to greater swings in temperature on land.
Responses
The oceans could absorb less heat, leading to a more steady temperature on land.
The oceans could absorb less heat, leading to a more steady temperature on land.
The oceans could absorb more heat, leading to greater swings in temperature on land.
The oceans could absorb more heat, leading to greater swings in temperature on land.
The oceans could absorb more heat, leading to a more steady temperature on land.
The oceans could absorb more heat, leading to a more steady temperature on land.
The oceans could absorb less heat, leading to greater swings in temperature on land.
The oceans could absorb less heat, leading to greater swings in temperature on land.
Answers
GPT-4o mini
If the specific heat capacity of water were smaller than it is, the correct response would be:
**The oceans could absorb less heat, leading to greater swings in temperature on land.**
This is because a lower specific heat capacity means that water can change temperature more rapidly in response to heat input or removal, resulting in less regulation of temperature and greater fluctuations on land.
**The oceans could absorb less heat, leading to greater swings in temperature on land.**
This is because a lower specific heat capacity means that water can change temperature more rapidly in response to heat input or removal, resulting in less regulation of temperature and greater fluctuations on land.