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the
CLIMATOLOGICAL STATIONS
Are categorized by the World Meteorological
Organization (WMO) as “principal and
ordinary; precipitation stations for specific
purposes. In the US, official climatological
records are collected from a variety of
stations, and observations are taken both paid
and unpaid observers. Daily accumulated
precipitation and maximum and minimum
temperature are measured at almost all
stations.
1. The principal climatological station network
for local climatological data (LCD) stations
defines climate for about 275 major cities and
towns.
The major climate –observing networks now operated by U.S national
Oceanic and Atmospheric Administration (NOAA) include the
following:
2. The co-op network defines the baseline
climate for the United States using about 5200
temperature stations and 7400 precipitation
stations.
The major climate –observing networks now operated by U.S national
Oceanic and Atmospheric Administration (NOAA) include the
following:
3. The hourly precipitation data (HPD) network
about 3000 stations establishes baseline rainfall
records for hydrologic purposes.
The major climate –observing networks now operated by U.S national
Oceanic and Atmospheric Administration (NOAA) include the
following:
4. The historical climate network (HCN) of 1215
temperature and precipitation stations is definite
network for documenting climate variations
and change.
The major climate –observing networks now operated by U.S national
Oceanic and Atmospheric Administration (NOAA) include the
following:
Standard medium sized
Cotton Region shelter
for housing temperature
and humidity sensors.
Height of the shelter is 4
ft. (1.12 m). Height of
the thermometers is
approximately 5.5 ft.
(1.68m)
and
The smaller plastic
shelter houses the
newer thermistor-based
maximum-minimum
temperature system
(MMTS) of the U.S.
National Weather
Service.
INSTRUMENTATION
The World Meteorological Organization
(WMO) has established requirements for
instrument shelters in which
temperature and humidity sensors are
housed. The National Weather service
has described the shelter, and provided
instructions for the exposures and
installation of its instrument.
INSTRUMENTATION
In addition to the standard mercury
thermometer and maximum and
minimum thermometers, temperature
sensors are available that use
thermocouples, resistance elements,
thermistors, and electric diodes and
transistors.
WIND MEASUREMENT
Wind is simply air in motion relative to
the surface of the earth. The standard
level for wind measurements is 10m
(32.8ft) above the ground over level
open terrain, but many observations are
taken at nonstandard levels. This creates
serious problems of homogeneity, since
the wind typically increase rapidly
through the lowest few meters of the
atmosphere.
It has its own dynamic characteristics.
The choice of the measurement technique depends on
the application.
STANDARD WIND VANES
WIND INSTRUMENTS
PROPELLER ANEMOMETERS
CUP ANEMOMETERS
RADIATION MEASUREMENT
Surface measurements of radiation
is far less common and more difficult
than measurements of the standard
meteorological parameters.
Consequently, the quality of the
climatological radiation data is less
reliable. Instruments for measuring
radiation are designed to measure the
intensity of radiant energy over broad or
narrow spectral band.
RADIATION MEASUREMENT
the radiation fluxes of interest
maybe divided into fluxes with
wavelength less than 4. 0µm (short-wave
solar radiation) and fluxes whose
wavelength is more than 4. 0µm (long
wave terrestrial radiation). The short
wave solar radiation can in turn be
subdivided into ultraviolet (uv, between
.2 and 0.38µm), visible (0.38 to 0.75µm),
and infrared (greater than 0.75µm
radiation).
RADIATION MEASUREMENT
The generic term radiometer refers to
any instrument for measuring radiation,
regardless of its special characteristics
and its mode of operation. The WMO
classification of radiation instruments
identifies five basic types.
NET RADIOMETER
PYRHELIOMETERPYRANOMETER
PYRRADIOMETER PYRGEOMETER
NET
PYRRADIOMETER
RADIATION INSTRUMENTS
Measures global solar radiation- that is, the short-wave radiation
received on a horizontal surface from sun and sky. Use of a
masking device to screen out the sun’s direct beam allows
measurement of the diffuse component of solar radiation.
PYRANOMETER
NET RADIOMETER
PYRHELIOMETERPYRANOMETER
PYRRADIOMETER PYRGEOMETER
NET
PYRRADIOMETER
RADIATION INSTRUMENTS
Measures only the direct beam component of the solar
radiation, i.e., the solar radiation received on a
horizontal surface
PYRHELIOMETER
NET RADIOMETER
PYRHELIOMETERPYRANOMETER
PYRRADIOMETER PYRGEOMETER
NET
PYRRADIOMETER
RADIATION INSTRUMENTS
Measures the total short-wave and long-wave
radiation incident on a horizontal plane.
PYRRADIOMETER
NET RADIOMETER
PYRHELIOMETERPYRANOMETER
PYRRADIOMETER PYRGEOMETER
NET
PYRRADIOMETER
RADIATION INSTRUMENTS
Measures the long-wave atmospheric radiation on a
horizontal upward-facing black surface at ambient air
temperature.
PYRGEOMETER
NET RADIOMETER
PYRHELIOMETERPYRANOMETER
PYRRADIOMETER PYRGEOMETER
NET
PYRRADIOMETER
RADIATION INSTRUMENTS
Measures total (short-wave and long-wave) net
radiation lux through a horizontal plane
NET PYRRADIOMETER AND NET
RADIOMETER
RADIATION MEASUREMENT
In addition to these five general
terms, trade names are often attached to
specific instruments. To ensure the
reliability and compatibility of radiation
measurements on an international and
national scale, the WMO has established
a system of world, regional, and national
centers that provide facilities, maintain
equipment, and conduct comparisons.
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Documenting the Recent Climate

  • 1. the
  • 2. CLIMATOLOGICAL STATIONS Are categorized by the World Meteorological Organization (WMO) as “principal and ordinary; precipitation stations for specific purposes. In the US, official climatological records are collected from a variety of stations, and observations are taken both paid and unpaid observers. Daily accumulated precipitation and maximum and minimum temperature are measured at almost all stations.
  • 3. 1. The principal climatological station network for local climatological data (LCD) stations defines climate for about 275 major cities and towns. The major climate –observing networks now operated by U.S national Oceanic and Atmospheric Administration (NOAA) include the following:
  • 4. 2. The co-op network defines the baseline climate for the United States using about 5200 temperature stations and 7400 precipitation stations. The major climate –observing networks now operated by U.S national Oceanic and Atmospheric Administration (NOAA) include the following:
  • 5. 3. The hourly precipitation data (HPD) network about 3000 stations establishes baseline rainfall records for hydrologic purposes. The major climate –observing networks now operated by U.S national Oceanic and Atmospheric Administration (NOAA) include the following:
  • 6. 4. The historical climate network (HCN) of 1215 temperature and precipitation stations is definite network for documenting climate variations and change. The major climate –observing networks now operated by U.S national Oceanic and Atmospheric Administration (NOAA) include the following:
  • 7.
  • 8. Standard medium sized Cotton Region shelter for housing temperature and humidity sensors. Height of the shelter is 4 ft. (1.12 m). Height of the thermometers is approximately 5.5 ft. (1.68m)
  • 9. and The smaller plastic shelter houses the newer thermistor-based maximum-minimum temperature system (MMTS) of the U.S. National Weather Service.
  • 10. INSTRUMENTATION The World Meteorological Organization (WMO) has established requirements for instrument shelters in which temperature and humidity sensors are housed. The National Weather service has described the shelter, and provided instructions for the exposures and installation of its instrument.
  • 11. INSTRUMENTATION In addition to the standard mercury thermometer and maximum and minimum thermometers, temperature sensors are available that use thermocouples, resistance elements, thermistors, and electric diodes and transistors.
  • 12. WIND MEASUREMENT Wind is simply air in motion relative to the surface of the earth. The standard level for wind measurements is 10m (32.8ft) above the ground over level open terrain, but many observations are taken at nonstandard levels. This creates serious problems of homogeneity, since the wind typically increase rapidly through the lowest few meters of the atmosphere.
  • 13. It has its own dynamic characteristics. The choice of the measurement technique depends on the application. STANDARD WIND VANES WIND INSTRUMENTS PROPELLER ANEMOMETERS CUP ANEMOMETERS
  • 14. RADIATION MEASUREMENT Surface measurements of radiation is far less common and more difficult than measurements of the standard meteorological parameters. Consequently, the quality of the climatological radiation data is less reliable. Instruments for measuring radiation are designed to measure the intensity of radiant energy over broad or narrow spectral band.
  • 15. RADIATION MEASUREMENT the radiation fluxes of interest maybe divided into fluxes with wavelength less than 4. 0µm (short-wave solar radiation) and fluxes whose wavelength is more than 4. 0µm (long wave terrestrial radiation). The short wave solar radiation can in turn be subdivided into ultraviolet (uv, between .2 and 0.38µm), visible (0.38 to 0.75µm), and infrared (greater than 0.75µm radiation).
  • 16. RADIATION MEASUREMENT The generic term radiometer refers to any instrument for measuring radiation, regardless of its special characteristics and its mode of operation. The WMO classification of radiation instruments identifies five basic types.
  • 18. Measures global solar radiation- that is, the short-wave radiation received on a horizontal surface from sun and sky. Use of a masking device to screen out the sun’s direct beam allows measurement of the diffuse component of solar radiation. PYRANOMETER
  • 20. Measures only the direct beam component of the solar radiation, i.e., the solar radiation received on a horizontal surface PYRHELIOMETER
  • 22. Measures the total short-wave and long-wave radiation incident on a horizontal plane. PYRRADIOMETER
  • 24. Measures the long-wave atmospheric radiation on a horizontal upward-facing black surface at ambient air temperature. PYRGEOMETER
  • 26. Measures total (short-wave and long-wave) net radiation lux through a horizontal plane NET PYRRADIOMETER AND NET RADIOMETER
  • 27. RADIATION MEASUREMENT In addition to these five general terms, trade names are often attached to specific instruments. To ensure the reliability and compatibility of radiation measurements on an international and national scale, the WMO has established a system of world, regional, and national centers that provide facilities, maintain equipment, and conduct comparisons.