Rayleigh-Bénard convection is a natural phenomenon that occurs when a layer of fluid is heated from below and cooled from above. The temperature difference generates patterns of rising warm plumes and descending cool currents, creating a display of fluid motion. In our video, we employ a technique known as 4D Laser-Induced Fluorescence (LIF) using a scanning method. This method involves using laser light to excite fluorescent molecules within the fluid. As these molecules emit light, their emissions are captured and analyzed in a four-dimensional space, which includes three spatial dimensions (x, y, z) and the fourth dimension representing time. This approach allows us to track the temperature variations within the Rayleigh-Bénard convection system over both space and time, offering a comprehensive and visually stunning representation of this natural phenomenon.