Why is evaporation considered an initial link of the water cycle?
Evaporation lifts water from the surface as vapour. This moisture later supports cloud and rainfall processes.
View question detailsMuft Shiksha™ एक 100% Free Education Portal है 🇮🇳, जिसका उद्देश्य Class 9–12 के हर विद्यार्थी तक High-Quality Education को पूरी तरह मुफ्त पहुँचाना है। 🇮🇳 हम मानते हैं कि अच्छी शिक्षा किसी student की आर्थिक स्थिति पर निर्भर नहीं होनी चाहिए। 🇮🇳 हर विद्यार्थी को वही Quality Study Material, MCQs, Quizzes, Exam Preparation, Concept-Based Learning और Bilingual Support मिलना चाहिए, जो आमतौर पर महंगी Coaching या Premium Platforms में मिलता है। Muft Shiksha™ 🇮🇳 इसी सोच के साथ बनाया गया है
SubjectsGeography
TOPIC PRACTICE
Up to 20 questions from this page. Select your focus, then start.
Evaporation lifts water from the surface as vapour. This moisture later supports cloud and rainfall processes.
View question detailsAfter evaporation from a water surface vapour enters air and cooling can cause condensation. This is the basic sequence of the subtopic.
View question detailsWhen temperature rises saturation capacity increases so the same moisture becomes a lower percentage. Understand the role of the denominator in relative humidity.
View question detailsCooler air can hold less water vapour so relative humidity rises. In closed space questions separate actual moisture from capacity.
View question detailsWhen air is near saturation the air temperature and dew point are nearly equal. Treat dew point depression as an indicator of moisture.
View question detailsStrong wind removes the saturated layer near the water surface and brings drier air. Renewal of air is important in evaporation.
View question detailsAbsolute humidity tells amount while relative humidity compares with saturation capacity. Separate the definitions by unit and percentage.
View question detailsRising air becomes saturated when cooling reaches the dew point. This is a key step in cloud formation.
View question detailsWarm air can hold more water vapour so the same moisture gives a lower percentage. This is how temperature changes relative humidity.
View question detailsDew forms by condensation of water vapour on a cool surface. Radiational cooling is greater on a clear night.
View question detailsIn humid and calm air the moisture gradient for sweat evaporation is low. Therefore sultriness is felt more.
View question detailsDust salt and smoke particles can act as condensation nuclei. Without them droplet formation may be difficult.
View question detailsRelative humidity compares the air moisture with its maximum capacity. Do not treat it as a certain chance of rainfall.
View question detailsFog forms when water vapour condenses into tiny droplets near the surface. Identify cooling and moisture near the ground together.
View question detailsEvaporation absorbs latent heat so it can produce a cooling effect. Remember the example of drying sweat.
View question detailsDry lower air can evaporate falling droplets. In rainfall questions also check the air between cloud and ground.
View question detailsEvapotranspiration is the combined measure of moisture loss from land and plants. In water budget treat it as moisture output.
View question detailsCold dense air can collect in valleys and bring near surface saturation. This can form valley fog.
View question detailsWhen they are equal (RH=\frac{e}{e_s}\times100) gives (100%). This is the condition of saturation.
View question detailsCloud droplets are initially very tiny so they can remain suspended. For rainfall droplets need to grow larger.
View question detailsQUIZ COMPLETE