If the surface is very hot but a stable air layer exists above why can convectional clouds be suppressed?
Upper stability can limit convective uplift. Exam tip: check atmospheric stability along with surface heating.
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.
Upper stability can limit convective uplift. Exam tip: check atmospheric stability along with surface heating.
View question detailsDrizzle is falling precipitation of small liquid drops. Exam tip: separate falling small drops from suspended droplets.
View question detailsLarge drops can grow further by collision and coalescence. Exam tip: remember the idea of coalescence.
View question detailsEvaporation of drops in lower air can reduce surface rainfall. Exam tip: separate cloud precipitation from surface measurement.
View question detailsHeight and form identify clouds like cirrus stratus and cumulus. Exam tip: read both clues together.
View question detailsIn mixed clouds ice crystal growth can strengthen precipitation. Exam tip: keep mixed cloud processes in mind.
View question detailsRain shadow is linked with long-term rainfall deficiency. Exam tip: distinguish one event from general climate.
View question detailsPartial melting can form mixed precipitation. Exam tip: read the lower thermal layers carefully.
View question detailsMore humid air can saturate with less cooling and form a lower cloud base. Exam tip: link humidity and cloud base.
View question detailsDescending warm air is linked with rain shadow and dryness. Exam tip: connect adiabatic warming with leeward dryness.
View question detailsCumulonimbus can have strong uplift and mixed particles causing stormy weather. Exam tip: remember hazards of storm clouds.
View question detailsUpdrafts can keep drops in the cloud for a while and increase growth. Exam tip: understand the balance between fallable size and updraft.
View question detailsConvectional rain can be intense over a small area. Exam tip: connect local intensity with convection.
View question detailsWarm lower air melts ice crystals. Exam tip: check lower air temperature for ground precipitation.
View question detailsCloud presence and precipitation are different conditions. Exam tip: separate cloud cover and precipitation.
View question detailsHigh cirrus clouds are generally made of ice crystals. Exam tip: connect high fibrous clouds with ice crystals.
View question detailsIn storm clouds liquid drops and ice particles can grow together. Exam tip: understand mixed phase and vertical motion.
View question detailsLower air can change both form and amount of precipitation. Exam tip: see the effect of the whole atmospheric column.
View question detailsMoisture distributed over more particles can create more small droplets. Exam tip: understand water content and particle number relation.
View question detailsThe leeward area can become relatively dry due to rain shadow. Exam tip: remember relation between relief and climate.
View question detailsQUIZ COMPLETE