Step 1: Why land-sea temperature differences arise.
Water has a much higher specific heat capacity compared to soil/rock. This means:
- The sea heats up and cools down more slowly.
- Land heats up and cools down quickly in response to solar radiation.
Step 2: Resulting thermal contrast.
- Daytime: Land surface warms much faster → land air becomes hotter → lower pressure → sea breeze (cool moist air from sea to land).
- Seasonal: In summer, the Indian subcontinent heats much more strongly than the ocean → strong land-sea pressure gradient → drives monsoon circulation (moist southwesterlies from ocean to land).
Step 3: Eliminate other options.
- (A) Cloud cover differences exist but are consequences, not the cause.
- (B) Albedo differences are smaller compared to heat capacity effects.
- (D) Surface roughness affects turbulence and drag, not large-scale temperature contrast.
Final Answer:
\[
\boxed{\text{Difference in the specific heat capacities between the land and the sea}}
\]