Examoogle
ExamsTest SeriesCBATRank CheckPrevious Year PapersPassBook StoreMy BooksAI Tutor
ЁЯЫТ0
рдЕA
Examoogle

India's most trusted platform for competitive exam PDF books. Expert-authored, watermark-protected, instant access.

Exams & Practice
All Exams & SyllabusMock Test SeriesPrevious Year PapersPractice Questions (MCQs)Recruitment Notifications
Quick Links
Examoogle AI TutorExam NewsBook StoreMy BooksLogin / Sign Up
Support
About UsRefund PolicyPrivacy PolicyTerms of UseContact Us
┬й 2026 Examoogle. India's #1 competitive exam AI tutor.
ЁЯФТ SSL SecuredЁЯУ▒ UPI AcceptedЁЯз╛ GST Invoice
Examoogle

Join 60,000+ competitive exam aspirants

or with email
By continuing, you agree to ourTerms of Service&Privacy Policy
Your Cart
SubtotalтВ╣0
TotalтВ╣0
Examoogle тАв User тАв info@examoogle.com тАв EE-2024-8821
Chapter 1 of 12 тАв Page 1 of 248ЁЯФТ Protected PDF тАв Watermarked
Back to Practice Questions
CivilWater Resources Management
PrevNext

When temperature is high, evaporation and runoff is......

A

evaporation is high and runoff is high

B

evaporation is high and runoff is low

C

evaporation is low and runoff is low

D

evaporation is low and runoff is high

Correct Answer

тЪЩя╕П TE тАв Technical Concept & PrincipleCivilWater Resources Management
Option B

evaporation is high and runoff is low

Quick Summary:

High temperature increases the rate of evaporation from water bodies and soil surfaces due to greater energy availability for phase change. Concurrently, since evaporation is an abstraction from the total precipitation, the net water available to form surface runoff is reduced, resulting in low runoff.

тЪЩя╕ПTETechnical SolutionConcept & Principle
ЁЯТб Explanation

High temperature increases the rate of evaporation from water bodies and soil surfaces due to greater energy availability for phase change. Concurrently, since evaporation is an abstraction from the total precipitation, the net water available to form surface runoff is reduced, resulting in low runoff.

ЁЯФв Key Formulas

E=KeтЛЕ(esтИТea)E = K_e \cdot (e_s - e_a)E=KeтАЛтЛЕ(esтАЛтИТeaтАЛ) тАФ where EEE is evaporation, ese_sesтАЛ is saturation vapor pressure (highly temperature-dependent), and eae_aeaтАЛ is actual vapor pressure.

Q=PтИТEтИТ╬ФSQ = P - E - \Delta SQ=PтИТEтИТ╬ФS тАФ where QQQ is runoff, PPP is precipitation, and ╬ФS\Delta S╬ФS is storage change.

тЪЩя╕П Working Principle

The principle is governed by the energy balance in the hydrologic cycle. When temperature rises, the vapor pressure deficit increases, accelerating the latent heat of vaporization process. Because evaporation acts as a depletion mechanism, high rates of vapor loss from a catchment leave less water to fill surface depressions and exceed infiltration capacities, thereby reducing the volume of surface runoff.

ЁЯУМ Key Points
  • тЦ╕

    Evaporation is directly proportional to temperature due to the Clausius-Clapeyron relation increasing saturation vapor pressure.

  • тЦ╕

    Runoff is the residual of precipitation after accounting for evaporation and infiltration.

  • тЦ╕

    Higher temperatures typically promote increased infiltration rates if the soil remains moist, further reducing surface runoff.

тЬЕ Advantages
  • тЦ╕

    High temperature aids in faster drying of agricultural fields.

  • тЦ╕

    Reduces water logging risks in poorly drained areas.

тЭМ Disadvantages / Limitations
  • тЦ╕

    Reduces storage capacity of reservoirs through high evaporative loss.

  • тЦ╕

    Decreases water availability for downstream irrigation and municipal use.

ЁЯЫая╕П Applications / Uses
  • тЦ╕

    Hydrological modeling for catchment yield analysis.

  • тЦ╕

    Reservoir management and climate change impact assessments.

ЁЯУД Additional Information
  • тЦ╕

    In arid regions, extreme temperatures often lead to high evaporation rates, rendering runoff almost zero during summer months.

  • тЦ╕

    Option A is incorrect because high evaporation consumes the potential runoff. Option C and D are incorrect as they defy the fundamental thermodynamic relationship between temperature and evaporation.

ЁЯУК Diagram / Illustration
Hydrologic Temperature Impact
TтЖСтАЕтАКтЯ╣тАЕтАКEтЖСT \uparrow \implies E \uparrowTтЖСтЯ╣EтЖС
TтЖСтАЕтАКтЯ╣тАЕтАКRтЖУT \uparrow \implies R \downarrowTтЖСтЯ╣RтЖУ
Where EEE: Evaporation, RRR: Runoff
TTT: Temperature
тЬЕ

B is correct тАФ High temperatures enhance evaporative loss, leaving significantly less water available as surface runoff.

Core Concepts Used
Click any tag to open in AI Tutor
Hydrologic Cycle Evapotranspiration Surface Runoff Dynamics
ЁЯТб EXAM TIP

Always remember that in the water balance equation P=R+E+IP = R + E + IP=R+E+I, EEE (evaporation) and RRR (runoff) compete for the same input PPP (precipitation).

Related Questions

CivilWater Resources Management
Dicken's formula for finding discharge is
CivilWater Resources Management
Check dam's top width is find by
CivilWater Resources Management
Remedial measurment to minimise water losses are
CivilWater Resources Management
Point to be consider during site selection of check dam are..
CivilWater Resources Management
Method of rainwater harvestings are..

Discussion (0)

Loading discussion...
PrevNext