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          <TD align=3Dmiddle width=3D"102%"><FONT=20
            face=3Darial,helvetica,verdana,sans-serif color=3D#ffffff=20
            size=3D+3><B>Falmouth Monthly Climate=20
      Reports</B></FONT></TD></TR></TBODY></TABLE></TD></TR>
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          <TD bgColor=3D#ffffff colSpan=3D2><FONT=20
            face=3Darial,helvetica,verdana,sans-serif>Contact: <A=20
            href=3D"mailto:rpayne@whoi.edu">Richard E. Payne</A>, ext. =
2550
            <P>
            <H3>Definition of parameters on monthly climatological data=20
            reports</H3>
            <P>
            <TABLE bgColor=3D#ffffff border=3D1>
              <TBODY>
              <TR>
                <TD><B>Column</B></TD>
                <TD><B>Units</B></TD>
                <TD><B>Description</B></TD></TR>
              <TR>
                <TD>DAY</TD>
                <TD>&nbsp;</TD>
                <TD>Day of the month</TD></TR>
              <TR>
                <TD>DAYNO</TD>
                <TD>&nbsp;</TD>
                <TD>Year day number</TD></TR>
              <TR>
                <TD>SORADM</TD>
                <TD>watt-hours/m<SUP>2</SUP></TD>
                <TD>Daily total of observed vertical solar energy =
flux</TD></TR>
              <TR>
                <TD>SORADC</TD>
                <TD>watt-hours/m<SUP>2</SUP></TD>
                <TD>Daily total of observed vertical solar energy flux =
with no=20
                  atmosphere (calculated)</TD></TR>
              <TR>
                <TD>AT</TD>
                <TD>Dimensionless</TD>
                <TD>Atmospheric transmittance =3D =
SORADM/SORADC</TD></TR>
              <TR>
                <TD>NOONALT</TD>
                <TD>Degrees</TD>
                <TD>Altitude of sun above horizon at solar =
noon</TD></TR>
              <TR>
                <TD>TMAX</TD>
                <TD>Deg F</TD>
                <TD>Maximum air temperature during 24 hour =
period</TD></TR>
              <TR>
                <TD>TMIN</TD>
                <TD>Deg F</TD>
                <TD>Minimum air temperature during 24 hour =
period</TD></TR>
              <TR>
                <TD>DD65</TD>
                <TD>Deg F</TD>
                <TD>Heating degree day total for house maintained at 70 =
deg=20
                  F<BR>DD65 =3D (TMAX + TMIN)/2 - 65</TD></TR>
              <TR>
                <TD>DD60</TD>
                <TD>Deg F</TD>
                <TD>Heating degree day total for house maintained at 65 =
deg=20
                  F<BR>DD60 =3D (TMAX + TMIN)/2 - 60</TD></TR>
              <TR>
                <TD>PRECIP</TD>
                <TD>Inches</TD>
                <TD>Precipitation in 24 hour =
period</TD></TR></TBODY></TABLE>
            <H3>Comments on measurements</H3>Solar radiation =
measurements are=20
            made with an Eppley PSP pyranometer mounted on the roof of =
the Clark=20
            Building, Quissett Campus, Woods Hole Oceanographic =
Institution. The=20
            output signal of the sensor is sampled at 10 second =
intervals and=20
            averaged over an hour by a Campbell data logger. The hourly =
totals=20
            have been archived since 1991. Daily totals are computed =
from the=20
            hourly totals and have been archived since 1975.=20
            <P>TMAX, TMIN, and PRECIP are recorded by Falmouth Water =
Department=20
            employees at the town pumping station located on the shore =
of Long=20
            Pond, the town reservoir. Beacuse this is an inland site, =
about 1.5=20
            miles from the shore of Buzzards Bay, air temperatures may =
differ=20
            considerably from temperatures at shore sites. The =
thermometers have=20
            not been calibrated since they were purchased in 1960 and =
their=20
            absolute accuracy cannot be vouched for. TMAX and TMIN have =
been=20
            recorded since 1960, PRECIP since 1966. All data are =
archived by=20
            Dick Payne (Ext 2550).=20
            <P>
            <H3>Atmospheric Transmittance</H3>Solar radiation received =
at the=20
            earth's surface can vary because of clouds, latitude, time =
of year,=20
            and time of day. If we consider only daily totals we =
eliminate the=20
            time of day. Because of the dependence on latitude and date, =
daily=20
            totals cannot be compared directly from one place and time =
to=20
            another but the dependence on latitude and date can be =
compensated=20
            for mathematically. Knowing a few astronomical parameters we =
can=20
            compute the amount of solar radiation which would fall on =
the=20
            earth's surface at a given location and date. If we compute =
it for=20
            Woods Hole and divide our measured daily totals by these =
computed=20
            daily totals, we get an index for each day which has a value =
between=20
            0 and about 0.75. This index is called the atmospheric =
transmittance=20
            (AT). A clear day yields an index of about 0.75; a very =
cloudy day=20
            might have an index of 0.1. This index changes primarily =
with the=20
            effects of the atmosphere (clouds, water vapor) but has the =
effects=20
            of latitude and date removed. This index can then be used to =
compare=20
            atmospheric effects at one location with those at another =
and one=20
            time of year with another. </FONT></TD></TR>
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