Surface Hydrology 1: Precipitation Flashcards

1
Q

What is the significance of a hyetograph?

A

A hyetograph is a plot of rainfall (precipitation) over time, useful for analyzing rainfall intensity and patterns

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2
Q

What are the main processes that lead to vertical movement of air?

A

Convection: Local heating of surface air.
Orographic ascent: Air forced over a mountain.
Shear ascent: Wind shear causing turbulence.
Frontal ascent: Collision of air masses leading to uplift.

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3
Q

What is relative humidity, and how is it calculated?

A

Relative humidity r = e_d / e_a × 100, where e_d is the actual vapor pressure and e_a is the saturation vapor pressure.

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4
Q

What is the maximum amount of water vapour an air parcel can hold dependent on?

A

Temperature

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5
Q

When does an air parcel become saturated?

A

Dew point

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6
Q

What are the key types of manual rain gauges?

A

Common types include the Met Office Mk 2, Snowdon, Octopent, and Bradford gauges.

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7
Q

When does condensation happen?

A

When air masses are cooled down until they reach their dew point

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8
Q

What is absolute humidity?

A

The mass of water vapour per unit volume of air

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9
Q

What is a tipping bucket rain gauge, and how does it work?

A

A tipping bucket rain gauge measures rainfall by collecting water in a small bucket, which tips when a set amount of water is collected, recording each tip.

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10
Q

How do manual gauges vary?

A
  • Orifice diameter
  • Height above ground
  • Shape
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11
Q

What is the role of weather radar in measuring precipitation?

A

Weather radar measures backscattered microwave radiation from water droplets, providing spatial precipitation data. Uses a narrow beam

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12
Q

What factors influence the accuracy of rain gauge measurements?

A

Errors can arise from airflow deflection around the gauge (upward or downward), leading to inaccurate readings

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13
Q

How do satellites measure precipitation?

A

Satellites use active and passive microwave sensors and infrared data to measure cloud properties and precipitation, as seen in systems like the Global Precipitation Measurement Mission.

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14
Q

Why is spatial interpolation necessary for precipitation data?

A

Precipitation is measured at points, so interpolation is needed to estimate the total flux over a catchment area, which is critical for water balance calculations.

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15
Q

What are isohyets, and what is their purpose?

A

Isohyets are lines of equal precipitation, drawn by hand or software, used to estimate spatial precipitation patterns in a catchment. Accurate but subjective

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16
Q

What is the intensity-duration-frequency (IDF) curve?

A

An IDF curve relates the intensity, duration, and frequency of rainfall events, which is important for storm analysis and flood risk assessment.

17
Q

What makes it difficult to detect trends in rainfall?

A

The inherent stochastic nature of precipitation

18
Q

What is kriging, and how is it used in hydrology?

A

Kriging is a statistical method for interpolating point observations, commonly used in Geographic Information Systems (GIS) for spatial analysis of precipitation data.

19
Q

What is the importance of rainfall frequency analysis?

A

Rainfall frequency analysis examines both the magnitude and duration of rainfall events, which helps predict the likelihood of extreme weather events like floods

20
Q

What is the assumption that can be made for IDF curves?

A

Precipitation can represented as a statistical phenomenon with stationary characteristics -> may be invalidated by climate change