Surface Hydrology 1: Precipitation Flashcards
What is the significance of a hyetograph?
A hyetograph is a plot of rainfall (precipitation) over time, useful for analyzing rainfall intensity and patterns
What are the main processes that lead to vertical movement of air?
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.
What is relative humidity, and how is it calculated?
Relative humidity r = e_d / e_a × 100, where e_d is the actual vapor pressure and e_a is the saturation vapor pressure.
What is the maximum amount of water vapour an air parcel can hold dependent on?
Temperature
When does an air parcel become saturated?
Dew point
What are the key types of manual rain gauges?
Common types include the Met Office Mk 2, Snowdon, Octopent, and Bradford gauges.
When does condensation happen?
When air masses are cooled down until they reach their dew point
What is absolute humidity?
The mass of water vapour per unit volume of air
What is a tipping bucket rain gauge, and how does it work?
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.
How do manual gauges vary?
- Orifice diameter
- Height above ground
- Shape
What is the role of weather radar in measuring precipitation?
Weather radar measures backscattered microwave radiation from water droplets, providing spatial precipitation data. Uses a narrow beam
What factors influence the accuracy of rain gauge measurements?
Errors can arise from airflow deflection around the gauge (upward or downward), leading to inaccurate readings
How do satellites measure precipitation?
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.
Why is spatial interpolation necessary for precipitation data?
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.
What are isohyets, and what is their purpose?
Isohyets are lines of equal precipitation, drawn by hand or software, used to estimate spatial precipitation patterns in a catchment. Accurate but subjective