Step 1: Understanding the Concept:
Microwave remote sensing uses electromagnetic radiation with wavelengths ranging from $1\text{ mm}$ to $1\text{ m}$ (frequencies from $0.3$ to $300\text{ GHz}$).
Because of these longer wavelengths, microwaves can penetrate clouds, haze, and rain, allowing for all-weather, day-and-night imaging.
Step 3: Detailed Explanation:
Let us analyze each of the monitoring applications:
(A) Soil moisture:
The dielectric constant of water ($\approx 80$) is much higher than that of dry soil ($\approx 3 - 4$).
Microwaves are highly sensitive to these dielectric changes, making them the primary tool for mapping surface soil moisture.
(B) Canopy structure:
Microwaves can penetrate vegetative canopies.
The backscattered signal provides information on leaf area index (LAI), branch orientation, and canopy biomass.
(C) Snow cover:
Microwaves can penetrate snowpacks, allowing researchers to measure snow water equivalent (SWE) and map snow-covered areas.
(D) Moisture profiling in the atmosphere:
Satellite microwave sounders measure emissions from atmospheric water vapor to construct vertical moisture and temperature profiles.
(E) Ocean circulation:
Microwaves are used in radar altimetry to measure sea surface height, which helps map ocean currents and circulation patterns.
Step 4: Final Answer:
Microwave remote sensing is highly useful for all five applications (A, B, C, D, and E).
This corresponds to Option (D).