The air temperature above coastal areas is profoundly influenced by the large specific heat of water. One reason is that the energy released when `1m^3` of water cools by `1^@C` will raise the temperature of a much larger volume of air by `1^@C`. Find this volume of air. The specific heat of air is approximately `1 kJ//kg^@C`. Take the density of air to be `1.3 kg//m^3`.

Explanation

To solve the problem, we need to find the volume of air that can be heated by 1 °C when 1 m³ of water cools by 1 °C. We will follow these steps:

### Step 1: Calculate the mass of 1 m³ of water
The density of water is approximately \( \rho_{water} = 1000 \, \text{kg/m}^3 \). Therefore, the mass \( m \) of 1 m³ of water is given by:

\[ m = \rho_{water} \times V_{water} \]
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