Diverse Environmental Systems
In this week’s field exercise we will be returning to Nottingham County
Park to measure the net radiation at
several different sites. The net
radiation is an extremely important atmospheric variable because the net
radiation at the earth’s surface provides the energy needed for processes such
as warming the earth’s surface, evaporation, plant transpiration, diverse
chemical and biological processes, etc.
All objects (that have temperatures
above absolute zero; 0 K) emit radiation of some type. ALL OBJECTS including you, your classmates,
the computer screen that you’re looking at right now, EVERYTHING.
The character of radiation that is emitted by an object is dependent upon
the temperature of the object. Two very
important formulae relate the temperature of an object to the amount and
wavelength of the radiation that is emitted by the object.
Steffan-Boltzman Law: E = sT4
Wien’s Displacement Law: l = C / T (K)
To measure the net radiation we will
need to measure two types of radiation common to the earth system; shortwave and longwave
radiation.
Shortwave radiation is the type of radiation that comes from the sun. This radiation is commonly assumed to have a wavelength (l) of between 0.2 mm to 2.0 mm (visible light has wavelengths of between 0.4 mm to 0.7 mm).
Longwave radiation is the radiation that comes from the majority of
objects at the earth’s surface (soil, plants, animals, humans, rock, water,
etc.). The earth’s atmosphere also
gives off longwave radiation. This radiation is typically assumed to have a
wavelength of between 2.0 mm to 40 mm (most objects, including humans give off radiation
at about 10 mm).
To measure the shortwave radiation we
will be using an instrument called a pyranometer. We will need to measure the shortwave
radiation coming toward the earth’s surface (incoming shortwave radiation) and
the shortwave radiation that is reflected by the earth’s surface (outgoing
shortwave radiation). Thus, we will be
using two pyranometers, one facing upward (measuring incoming shortwave
radiation) and one facing downward (measuring outgoing shortwave radiation).
To measure longwave radiation we will
be using a different instrument called an infrared
temperature gun. Once again, we will need to measure the radiation moving from the
earth toward the atmosphere (outgoing longwave radiation) and from the
atmosphere toward the earth (incoming longwave radiation).
We will be measuring
the net radiation at three locations within Nottingham Park. These locations include a deciduous forest
environment, a “savannah location” and a landscape cleared by humans. At each station we will take measurements of
the following radiation variables every minute for a 15-minute period:
1)
Rsd - using pyranometer
#1
2)
Rsu - using pyranometer
#2
4)
“sky” IR temperature using the IR
temperature “gun”
5) surface IR temperature using the IR
temperature “gun”
6)
the time of the observations
(approximate)
7) sky conditions
8) the percentage of the sky hemisphere
obstructed (estimate)
!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!
** Please calculate the albedo (A), using Rsd
and Rsu
** Please calculate the net radiation from
the equation:
Rn = (1-A)Rsd
+ Rld - Rlu
** Please compare and contrast the calculated
and measured net radiation values at each site.
!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!
Radiation Measurements Site #1
Sky Condition____________ Sky Obstructed________
Ob # Time |
SWR Down |
SWR Up |
Sky Temp |
Ground Temp |
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Radiation Measurements Site #2
Sky Condition____________ Sky Obstructed________
Ob # Time |
SWR Down |
SWR Up |
Air Temp |
Ground Temp |
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Radiation Measurements Site #3
Sky Condition____________ Sky Obstructed________
Ob # Time |
SWR Down |
SWR Up |
Air Temp |
Ground Temp |
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