Hydrology: Fundamentals, Precipitation, and Infiltration

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Comprehensive fill-in-the-blank flashcards covering the introduction to hydrology, the hydrologic cycle, precipitation measurement and spatial estimation methods, double mass analysis, and mathematical infiltration models (Horton, Philip, and Green-Ampt).

29 Terms

1
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Hydrology is concerned with the occurrence, movement, distribution, and properties of water on and below the __________ surface.

Earth's

2
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Hydrologists often use mathematical models and __________ to predict water movement and assess the impact of environmental changes on water resources.

Geographic Information Systems (GIS)

3
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The branch of hydrology that examines interactions between water and the atmosphere is known as __________.

hydrometeorology

4
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The branch of hydrology that studies groundwater in relation to geological formations is called __________.

hydrogeology

5
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Temporary storage occurring when precipitation is caught by vegetation, buildings, and other surfaces before reaching the ground is called __________.

interception

6
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The downward movement of infiltrated water through the soil and toward the groundwater zone is termed __________.

percolation

7
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Evapotranspiration is defined as the combined loss of water through evaporation and plant transpiration, represented by the relationship __________ = E+TE + T.

ET\text{ET}

8
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During plant transpiration, water vapor is released into the atmosphere through small pores in leaves known as __________.

stomata

9
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In warm clouds, droplets grow sufficiently large to fall as rain primarily through the __________ process.

collision-coalescence

10
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__________ lifting occurs when moist air encounters a mountain or elevated terrain and is forced upward, resulting in a wetter windward side and a drier leeward side.

Orographic

11
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Soft, opaque ice pellets formed when supercooled water droplets collect on snow crystals are called __________.

graupel

12
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A graphical representation of the variation of rainfall intensity over time during a storm event is called a(n) __________.

hyetograph

13
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A(n) __________ rain gauge records rainfall electronically by balancing a small container on a pivot that empties and triggers a count when filled to a certain level.

tipping bucket

14
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A rain gauge that estimates rainfall rate by detecting the interruption, scattering, or absorption of a light beam by falling raindrops is a(n) __________ rain gauge.

optical

15
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Lines drawn on a map connecting points of equal rainfall depth based on point rainfall data are called __________.

isohyets

16
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In the Thiessen polygon method, the areal rainfall is calculated as a weighted average using the Thiessen weight given by the formula Wi=W_i = __________.

AiA\frac{A_i}{A}

17
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Unlike Inverse Distance Weighting, Kriging models spatial correlation and calculates interpolation weights using a statistical function called a(n) __________.

variogram

18
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The relationship used to convert point rainfall depth (PPP_P) to an equivalent areal rainfall depth (PAP_A) over a watershed is PA=P_A = __________ ×PP\times P_P.

ARF\text{ARF}

19
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__________ analysis is a graphical technique used to check the consistency or homogeneity of rainfall records by plotting cumulative values against cumulative reference station values.

Double mass

20
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When adjusting an inconsistent rainfall record in double mass analysis to match the earlier slope m1m_1 from a later slope m2m_2, the correction factor is Cf=C_f = __________.

m1m2\frac{m_1}{m_2}

21
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The maximum rate at which a soil can absorb water under specific conditions is called the infiltration __________.

capacity

22
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In a double-ring infiltrometer, the outer ring is designed to minimize __________ water movement while the inner ring measures vertical infiltration.

lateral

23
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Horton's empirical infiltration equation expresses infiltration capacity as f(t)=f(t) = __________.

fc+(f0−fc)e−ktf_c + (f_0 - f_c)e^{-kt}

24
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In Philip's infiltration equation I(t)=St+AtI(t) = S\sqrt{t} + At, the parameter SS represents __________, which quantifies the soil's capacity to absorb water via capillary forces.

sorptivity

25
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Differentiating Philip's cumulative infiltration equation yields the infiltration rate formula f(t)=f(t) = __________.

S2t+A\frac{S}{2\sqrt{t}} + A

26
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The Green-Ampt model simplifies unsaturated infiltration by assuming the presence of a distinct, sharp __________ separating the fully saturated zone from the drier soil below.

wetting front

27
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In the Green-Ampt infiltration rate equation f(t)=K(1+ψΔθF(t))f(t) = K\left(1 + \frac{\psi\Delta\theta}{F(t)}\right), the variable ψ\psi represents the __________.

wetting front soil suction head

28
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Under the Green-Ampt model, surface ponding will occur only when rainfall intensity ii is __________ the saturated hydraulic conductivity KK.

greater than

29
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Under constant rainfall intensity ii exceeding KK, the Green-Ampt formula for calculating ponding time is tp=t_p = __________.

KψΔθi(i−K)\frac{K\psi\Delta\theta}{i(i - K)}