MEV 012: Unit 08 - Hydro-meteorology and Climate
UNIT 8: HYDROMETEOROLOGY AND CLIMATE
8.0 Introduction
Hydrometeorology
is the study of the transfer of water and energy between the land surface and
the lower atmosphere.
It combines
principles of meteorology, climatology, and hydrology to understand
precipitation, evaporation, evapotranspiration, soil moisture, river flow, and
groundwater dynamics.
With climate change influencing hydrological processes, hydrometeorological
data is essential for effective water resource planning, flood forecasting, and
environmental management.
8.1 Objectives
After
studying this unit, you will be able to:
·
Explain the structure and components of a hydrometric network.
·
Describe precipitation processes, types, and measurement methods.
·
Understand evaporation and evapotranspiration processes.
·
Estimate soil moisture content.
·
Identify river, lake, and groundwater types.
·
Understand the hydrological cycle and movement of water.
·
Assess the impact of climate change on hydrology.
8.2 Hydrometric Networks and
Catchment Morphology
8.2.1 Important Definitions
·
Catchment: The area
contributing surface runoff to a specific point.
·
Hydrometric
Station: A location where hydrological and meteorological measurements
are taken.
8.2.2 Components of
Hydrometric/Hydrological Network Design
·
Precipitation
stations
·
Streamflow
gauging stations
·
Evaporation
stations
·
Groundwater
observation wells
8.2.3 Impact of Climate Change on
Hydrology and Importance of Hydrometric Networks
·
Altered precipitation patterns and intensity.
·
Increased evapotranspiration due to higher temperatures.
·
Variability in river flows and groundwater recharge.
·
Essential role of networks in monitoring and predicting changes.
8.3 Precipitation
8.3.1 Occurrence of Precipitation
Formed
when moist air cools and condenses into water droplets that coalesce into rain,
snow, or other forms.
8.3.2 Types of Precipitation
·
Cyclonic
·
Convective
·
Orographic
8.3.3 Measurement of Precipitation
·
Rain gauges (standard,
tipping bucket, weighing type)
·
Radar and
satellite observations
8.4 Evaporation and Evapotranspiration
8.4.1 Evaporation
Process
by which water changes from liquid to vapour.
8.4.1.1
Measurement of Evaporation
·
Pan evaporimeters (Class A, ISI standard)
·
Energy balance and aerodynamic methods
8.4.2 Evapotranspiration
Combined
water loss from evaporation and transpiration by plants.
8.4.3 Types of Evapotranspiration
·
Potential ET
·
Actual ET
8.4.4 Factors Affecting
Evapotranspiration
·
Temperature, humidity, wind speed, solar radiation, vegetation
type.
8.4.5 Estimation of
Evapotranspiration
·
Penman-Monteith equation
·
Blaney–Criddle method
8.5 Soil Moisture
8.5.1 Estimation of Soil Moisture
·
Gravimetric method
·
Neutron probe
·
Time domain reflectometry
8.6 River Flow
Measurement
and analysis of the volume and rate of water movement in rivers.
8.7 Rivers, Lakes, and Groundwater
8.7.1 Rivers
8.7.1.1
Classification of Rivers
·
Perennial, intermittent, ephemeral.
8.7.2 Lakes
8.7.2.1
Classification of Lakes
·
Tectonic, volcanic, glacial, artificial.
8.7.3 Groundwater
8.7.3.1 Types
of Groundwater
·
Confined, unconfined, perched.
8.8 Occurrence of Surface Water
and Groundwater
8.8.1 Surface Water
8.8.1.1 Sources
of Surface Water
·
Rivers, lakes, reservoirs, glaciers.
8.8.2 Methods of Streamflow
Monitoring
·
Velocity–area method
·
Dilution techniques
·
Acoustic Doppler current profilers
8.8.3 Groundwater
8.8.3.1 Zones
of Underground Water
·
Zone of aeration
·
Zone of saturation
8.8.3.2
Aquifers and Their Types
·
Confined, unconfined, leaky, perched.
8.8.3.3 Sources
of Underground Water
·
Rainwater infiltration, seepage from rivers/lakes.
8.9 Movement of Water on the
Surface and Below the Surface
8.9.1 Hydrological Cycle
Continuous
circulation of water between atmosphere, land, and oceans.
8.9.2 Behavior of Rivers Due to
Silt and Sediments
·
Silt deposition altering river morphology.
·
Reduction in channel capacity and flow velocity.
8.9.3 Movement of Groundwater
8.9.3.1 Darcy’s
Law for Determination of Groundwater Velocity
Where
8.9.3.2
Groundwater Yield
Volume
of water that can be extracted sustainably from an aquifer.
8.10 Let Us Sum Up
Hydrometeorology
integrates climatic and hydrological processes. Understanding precipitation,
evaporation, soil moisture, and water movement is crucial for water management,
especially under climate change. Hydrometric networks are vital for monitoring,
forecasting, and sustainable resource use.
8.11 Keywords
·
Hydrometric
Network – System for collecting hydrological data.
·
Evapotranspiration – Combined
water loss from evaporation and plant transpiration.
·
Aquifer –
Underground layer of water-bearing rock.
·
Hydrological
Cycle – Continuous movement of water on, above, and below the Earth’s
surface.
·
Darcy’s Law – Equation
governing groundwater flow.
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