Microwave remote sensing, an indispensable earth observation technology, receives and analyzes signatures either transmitted or reflected from features using electromagnetic waves with wavelength primarily ranging from 1 mm to 100 cm. Microwave remote sensing can be divided into two categories, based on the type of sensor used: passive and active. The passive approach uses natural illumination energy emitted via either thermal or microwave radiation. The active approach, on the other hand, transmits its own energy toward earth; this interacts with the atmosphere and/or surface and reflects back toward the sensor. There are two types of data acquisition which are feasible through this technology, and techniques include the imaging systems of the microwave radiometer and side‐looking radar and the non‐imaging systems of the microwave scatterometer and altimeter. In the past half century, microwave remote sensing applications on ocean, land, atmosphere, and ice, for disaster mitigation, and even for archaeology and other areas of work have registered significant progress, particularly owing to their all‐weather, all‐day operational capability, which combines penetration and interferometry.