Why may daytime temperature decrease when less energy reaches Earth's surface?
With less insolation the surface heats less. Exam tip: connect surface temperature with received insolation.
Muft 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
पृथ्वी का ऊष्मा बजट
Class 11 Geography explores the heat budget of the Earth as the balance between incoming solar radiation and outgoing terrestrial radiation. Students learn how the atmosphere, land, oceans, clouds, and ice reflect, absorb, store, and redistribute heat, and why the Earth’s average temperature remains broadly stable. The topic connects this balance with the greenhouse effect, latitudinal differences in heating, and the movement of heat through the atmosphere and oceans.
TOPIC PRACTICE
Up to 25 questions from this page. Select your focus, then start.
With less insolation the surface heats less. Exam tip: connect surface temperature with received insolation.
At a natural level it helps maintain balanced temperature. Exam tip: distinguish natural and enhanced greenhouse effect.
Particles can change the direction and amount of incoming radiation. Exam tip: connect aerosols with radiation modification.
When the difference between incoming and outgoing energy changes temperature is affected. Exam tip: connect climate change with energy imbalance.
Ozone absorbs ultraviolet radiation and affects atmospheric energy balance. Exam tip: connect ozone with incoming radiation absorption.
Incoming radiation is solar shortwave and outgoing radiation is terrestrial longwave. Exam tip: remember direction and wavelength together.
Part of energy over a wet surface is used in evaporation. Exam tip: connect moisture with latent heat process.
Unequal heating creates pressure differences and winds. Exam tip: connect unequal heating with wind formation.
The atmosphere regulates heat and reduces extreme heating and cooling. Exam tip: understand atmosphere as a thermal blanket.
Thermal balance exists when Earth emits nearly as much energy as it receives. Exam tip: connect long-term balance with input-output equality.
Black asphalt absorbs more solar energy and reflects less. Exam tip: also connect asphalt with urban heat.
Atmosphere and oceans carry heat from surplus areas to deficit areas. Exam tip: connect horizontal transfer with global circulation.
In dry and clear conditions heating by day and cooling by night are rapid. Exam tip: connect desert range with low humidity.
Distribution of energy forms the basis of atmospheric conditions. Exam tip: treat heat budget as a foundation of weather and climate.
Clouds send the largest reflected share of incoming solar energy back to space. In exams remember cloud reflection as about twenty seven units.
The part directly reflected by the surface is small in total reflection. In exams remember surface reflection as about two units.
Particles in the atmosphere scatter some solar energy back toward space. In exams remember scattering share as about six units.
Total reflection is thirty five units so after twenty seven and six the surface part is two units. In exams solve it by subtraction.
Surface absorption later becomes the basis for emission of longwave energy. In exams link fifty one units with surface heating.
A small but important part of solar energy is absorbed in the atmosphere itself. In exams take atmospheric absorption as fourteen units.
The surface emits absorbed energy as longwave terrestrial radiation. In exams link direct outgoing energy with longwave radiation.
The atmosphere absorbs a large part of longwave energy emitted by the surface. In exams link thirty four units with atmospheric greenhouse absorption.
The atmosphere re radiates the energy it receives toward space. In exams add fourteen and thirty four to remember forty eight.
All returning energy parts together make hundred units. In exams remember total outgoing as thirty five plus seventeen plus forty eight.
Absorbed energy is ultimately balanced by longwave energy output. In exams remember sixty five absorption and sixty five heat output together.
QUIZ COMPLETE