सापेक्ष आर्द्रता

सापेक्ष आर्द्रता क्या है?

Relative humidity (RH) is temperature-dependent: the same amount of moisture gives higher RH at lower temperatures. This is why RH is often near 100% early morning (cool) and drops to 50-60% by afternoon (warm), even though the actual moisture content hasn’t changed. In tropical Southeast Asia, RH is typically 70-95% year-round, creating the persistent muggy feeling that characterises the climate.

मुख्य बिंदु

• उस तापमान पर अधिकतम के सापेक्ष हवा में नमी का प्रतिशत।
• श्रेणी: measurement