In the context of climate science, understanding feedback mechanisms is critical for predicting changes in the Earth's climate system, especially as these feedbacks can either amplify or dampen initial climate changes. Among these, cloud feedback and lapse-rate feedback are particularly significant, and their dynamics have implications even for sectors such as the construction industry, where climate-related hazards influence safety planning, structural design, and workplace conditions. Cloud feedback refers to the process by which changes in cloud cover, cloud type, or cloud altitude influence the Earth's energy balance and, consequently, surface temperatures. Clouds have a dual role in the climate system: they reflect incoming solar radiation back into space, which has a cooling effect, and they also trap outgoing infrared radiation, contributing to a warming effect. The net effect of clouds on the Earth's energy balance depends on cloud properties such as thickness, height, and geographic distribution. High-altitude clouds, like cirrus clouds, tend to trap more heat and have a net warming effect, while low-altitude clouds, such as stratocumulus, typically reflect sunlight and produce a cooling effect. When global temperatures rise, cloud properties may change, creating a feedback loop. If warming leads to an increase in high, thin clouds that trap more heat, the result is a positive feedback, amplifying the initial warming. Conversely, if low clouds increase, they could produce a negative feedback, mitigating temperature rise. In the construction industry, understanding cloud feedback is essential for assessing future climate risks. Changes in temperature and precipitation patterns influenced by cloud feedback can affect worksite conditions, the integrity of building materials, and the likelihood of extreme weather events such as storms, which pose safety hazards to construction workers. Proper scheduling, protective measures, and resilient construction practices require awareness of how cloud dynamics may alter local climates over time. Lapse-rate feedback, on the other hand, concerns the vertical temperature profile of the atmosphere and its response to surface warming. The lapse rate is the rate at which air temperature decreases with altitude. A critical principle of atmospheric thermodynamics is that the rate of temperature decrease with height is not uniform and depends on moisture content and convection processes. When the Earth's surface warms, the air near the surface heats up, and the lapse rate determines how quickly the temperature drops with elevation. In a warmer climate, the