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Reference documents
![](/web/20061120224411im_/http://www.osl.gc.ca/sgdo/images/px-rouge.gif) |
Variables and units |
VARIABLES AND UNITS
USED IN THE ODMS |
Data held in
the ODMS are usually archived in the units specified by the International
System of Units, commonly known by the French abbreviation “SI”
(Système International d'unités). However,
instruments frequently do not measure data in these same units,
making conversion necessary. In addition, many variables have traditionally
been recorded in non-SI units and their use remains common in the
scientific community. For the sake of simplicity, these traditional
units are archived (water column pressure in decibars is a good
example).
Below we give information on the most common variables measured,
the units they are reported in, and unit conversions (including
some units that were formerly used but that are now obsolete). The
list is not exhaustive; if additional information is needed, there
are many on-line sites available that are dedicated to unit conversion
(e.g., http://physics.nist.gov/cuu/index.html
or http://www.digitaldutch.com/unitconverter).
We also include methods for converting latitude and longitude to
decimal degrees and local time to GMT.
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TIME–SPACE INFORMATION |
Position
(archived in decimal degrees)
By convention, latitude north and longitude east are positive.
- degrees + (minutes.mm / 60) = decimal degrees
example: 45°45.0' W = –45.750°
- degrees + (minutes + (seconds.ss/60))/60 = decimal degrees
example: 45°30'30.0'' N = 45.50833°
- to convert decimal degrees to degrees minutes.mmm, multiply
the decimal portion by 60 to get decimal minutes
example: 45.2500°N = 45+(0.25*60) = 45°15.0'
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Time
(archived in UTC)
UTC (Universal Time Coordinate) or Z time (Z for zero meridian or
Zulu time). Before 1972, universal time was known as Greenwich Mean
Time (GMT), but this term is no longer in use. Convert local time
to UTC by adding the offset in the western hemisphere and subtracting
it in the eastern hemisphere. Don't forget that changing times around
midnight might also result in a change of the date.
-
Standard Time ![](/web/20061120224411im_/http://www.osl.gc.ca/sgdo/images/px-rouge.gif) |
Eastern
Atlantic
Newfoundland |
EST
AST
NST |
+5 h
+4 h
+3.5 h |
=GMT
=GMT
=GMT |
Daylight Time ![](/web/20061120224411im_/http://www.osl.gc.ca/sgdo/images/px-rouge.gif) |
Eastern
Atlantic
Newfoundland |
EDT
ADT
NDT |
+4 h
+3 h
+2.5 h |
=GMT
=GMT
=GMT |
examples : |
0800 EST +
5 hours = 1300 GMT |
|
2000 16 May EDT
+ 4 hours = 2000 17 May GMT |
To indicate local time, specify a positive offset west of 0°
longitude and a negative offset east of 0° longitude. For example,
to indicate Eastern Standard Time, one would specify –0500.
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ENVIRONMENTAL INFORMATION
(weather and sea conditions) |
Air temperature (archived in °C)
° C = (°F-32)*(5/9)
example: (50°F-32)*(5/9) = 10°C
Atmospheric pressure (archived in hectopascals,
hPa)
millibars (mb)
hPa
1 atm=101325 Pa = 760 mm Hg = 1013.25 hPa = 1013.25 mb = 29.921261
in Hg
in of mercury * 33.86388 = mb = hPa
Cloud cover (World Meteorological Organization
[WMO] code table 2700 for recording cloud amount)
To use this table, the sky is divided either into eighths (“okta”)
or tenths and the cloud cover is estimated.
Code
![](/web/20061120224411im_/http://www.osl.gc.ca/sgdo/images/px-rouge.gif) |
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Cloud
cover ![](/web/20061120224411im_/http://www.osl.gc.ca/sgdo/images/px-rouge.gif) |
0 |
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Zero |
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Zero |
1 |
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1 okta
or less, but not zero |
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1/10 or
less, but not zero |
2 |
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2 oktas |
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2/10 to
3/10 |
3 |
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3 oktas |
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4/10 |
4 |
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4 oktas |
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5/10 |
5 |
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5 oktas |
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6/10 |
6 |
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6 oktas |
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7/10 to
8/10 |
7 |
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7 oktas
or less, but not 8 oktas |
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9/10 or
more, but not 10/10 |
8 |
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8 oktas |
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10/10 |
9 |
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Sky
obscured, or cloud amount cannot be estimated |
![](/web/20061120224411im_/http://www.osl.gc.ca/sgdo/images/px-rouge.gif) |
Sea state (WMO code table 3700 for recording
sea state)
Code
![](/web/20061120224411im_/http://www.osl.gc.ca/sgdo/images/px-rouge.gif) |
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Description
![](/web/20061120224411im_/http://www.osl.gc.ca/sgdo/images/px-rouge.gif) |
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Wave height
(m) ![](/web/20061120224411im_/http://www.osl.gc.ca/sgdo/images/px-rouge.gif) |
0 |
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Calm-glassy |
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0 |
1 |
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Calm-rippled |
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0-0.1 |
2 |
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Smooth-wavelet |
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0.1-0.5 |
3 |
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Slight |
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0.5-1.25 |
4 |
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Moderate |
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1.25-2.5 |
5 |
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Rough |
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2.5-4 |
6 |
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Very rough |
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4-6 |
7 |
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High |
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6-9 |
8 |
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Very high |
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9-14 |
9 |
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Phenomenal |
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>14 |
![](/web/20061120224411im_/http://www.osl.gc.ca/sgdo/images/px-rouge.gif) |
Secchi disk depth (m)
A measure of water clarity
Wind speed estimation: the Beaufort Wind Scale
(marine)
The Beaufort Scale was originally developed in 1805 by Sir Francis
Beaufort as a system for estimating wind strengths without the use
of instruments. It is still in use for this same purpose as well
as to tie together various components of weather (wind strength,
sea state, observable effects) into a unified picture.
Even though the Beaufort Scale is not used in the ODMS
archive, we include it here to dispel any confusion between
it and the WMO code table 3700, which we use for describing sea
state.
Force
![](/web/20061120224411im_/http://www.osl.gc.ca/sgdo/images/px-rouge.gif) |
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Wind
speed ![](/web/20061120224411im_/http://www.osl.gc.ca/sgdo/images/px-rouge.gif) |
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Marine
Conditions ![](/web/20061120224411im_/http://www.osl.gc.ca/sgdo/images/px-rouge.gif) |
Knots |
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mph |
0 |
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<1 |
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<1 |
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Calm, sea
like a mirror |
1 |
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1-3 |
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1-3 |
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Light air,
ripples only |
2 |
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4-6 |
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4-7 |
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Light breeze,
small wavelets (0.2m), crests have a glassy appearance |
3 |
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7-10 |
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8-12 |
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Gentle
breeze, large wavelets (0.6m), crests begin to break |
4 |
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11-16 |
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13-18 |
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Moderate
breeze, small waves (1m), some white caps |
5 |
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17-21 |
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19-24 |
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Fresh breeze,
moderate waves (1.8m), many white caps |
6 |
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22-27 |
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25-31 |
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Strong
breeze, large waves (3m), probably some spray |
7 |
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28-33 |
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32-38 |
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Near gale,
mounting sea (4m) with foam blown in streaks downwind |
8 |
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34-40 |
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39-46 |
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Gale, moderately
high waves (5.5m), crests break into spindrift |
9 |
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41-47 |
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47-54 |
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Strong
gale, high waves (7m), dense foam, visibility affected |
10 |
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48-55 |
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55-63 |
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Storm,
very high waves (9m), heavy sea roll, visibility impaired. Surface
generally white |
11 |
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56-63 |
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64-73 |
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Violent
storm, exceptionally high waves (11m), visibility poor |
12 |
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64+ |
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74+ |
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Hurricane,
14m waves, air filled with foam and spray, visibility bad |
![](/web/20061120224411im_/http://www.osl.gc.ca/sgdo/images/px-rouge.gif) |
Wind speed (archived in m/s)
knots * 0.514 = m/s
Wind direction (degrees)
The wind direction is by convention the direction from which the
wind blows and is measured as degrees from true north.
0: wind from the north; 90: from the east; 180: from the south;
270: from the west
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PHYSICAL PROPERTIES |
The most common
physical variables held in the ODMS archive include:
Altimeter (m)
Distance of the instrument off-bottom
Conductivity (archived in S/m)
Siemens were formerly called “mho”; mho are still commonly
used. Siemens are the reciprocal of ohms: 1 ohm = 1/S.
Current components (m/s)
The north-south (V) component is positive toward the geographic
north.
The east-west (U) component is positive toward the east.
Current direction (degrees)
By convention, current direction is the direction toward which the
current flows, measured in degrees from true or magnetic north.
0: current flowing toward the north; 90: flowing toward the east;
180: flowing toward the south; 270: flowing toward the west
Current direction; magnetic declination (degrees)
The angle between the magnetic and geographical meridians at any
place, expressed in degrees east or west to indicate the direction
of magnetic north from true north
Density (archived in kg/m3)
Density of seawater
Density, sigma-t (archived in kg/m3)
Sigma-t = the density of seawater – 1000 kg/m3
Depth (m)
Descent rate (m/s) of the profiler (e.g., a ctd)
Fluorescence (archived in mg/m3)
An index of the amount of chlorophyll in the water
Oxygen (archived in mL/L)
The amount of oxygen dissolved in the seawater. It can be expressed
in many different units (mg/L, mL/L, µmol kg, % saturation;
see the next section for unit conversions). The unit used most frequently
is mL/L. The percent saturation corresponds to the measured value
divided by the value for 100% saturation of oxygen in seawater (calculated
from water temperature and salinity) multiplied by 100.
Oxygen sensor current (archived in µA)
Older oxygen sensors used sensor current and sensor temperature
to calculate dissolved oxygen
Oxygen sensor temperature (archived in °C)
Older oxygen sensors used sensor current and sensor temperature
to calculate dissolved oxygen
PAR radiation (Photosynthetically Active Radiation;
archived in µE/s/m2)
Units currently used include moles, einsteins (E), photons, and
quanta:
1 µmol/s/m2
1 µeinstein/s/m2
6.02*1017 photons/s/m2 = 6.02*1017 quanta/s/m2
Pressure (db, decibars)
Salinity (unitless)
The calculation of salinity is a ratio so there are no units. One
will frequently see salinity recorded in units of “PSU”
to indicate “practical salinity unit,” making reference
to the Practical Salinity Scale 1978 (PSS78).
Temperature (°C)
The calculation of temperature is based on the International Temperature
Scale of 1990 (ITS-90) or the International Practical Temperature
Scale of 1968 (ITPS-68)
° C (ITS-90) = °C (ITPS-68)/1.00024
Transmissometer (%)
Measurement of light transmission (index of the concentration of
suspended matter)
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SUBSTANCE CONCENTRATIONS
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Data from bottle
samples. The SI unit for the amount of a substance is mole, abbreviated
as "mol."
Dissolved oxygen (archived in mL/L; SI unit is
mmol/m3)
mL/L * 44.66 = mmol/m3
mL/L = mg/L * (1 mL/1.42903 mg)
mg/L = mL/L * 1.42903 mg/mL
mg/L
mg/kg
mg/L
ppm
Nutrients (archived in mmol/m3)
The most common nutrients measured are nitrite, nitrate + nitrite,
phosphate, silicate
µmol/L = mmol/m3
M
gram molecular weight per liter (or molar concentration)
µg-atoms/L
mg-atoms/m3
µM
µmol/L
µg/L = mg/m3
ppm
mg/L
ppb µg/L
µg/L / atomic mass = µg-atoms/L
µg/L / molecular mass = µM = µmol/L
Particulate matter
- unspecified or complex compounds (including chlorophyll) (precise
molecular mass unknown):
mg/m3 = µg/L
mg/L = g/m3
- POC (particulate organic carbon): (µg L)/12.01 = mmol/m3
(archived in mmol/m3)
- PON (particulate organic nitrogen): (µg L)/14.01 = mmol/m3
(archived in mmol/m3)
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QUALITY FLAGS (following
the Global Temperature-Salinity Pilot Project [GTSPP] system) |
0: No quality control
(QC) has been performed on the value
1: QC performed, value appears correct
2: QC performed, value appears inconsistent with other values
3: QC performed, value appears doubtful
4: QC performed, value appears erroneous
5: Value has been changed as a result of QC
6-8: Reserved for future use
9: Value of the parameter is missing
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MISCELLANEOUS |
1 degree of latitude
= 60 nautical miles
1 minute of latitude = 1 nautical mile = 1852 m
1 nautical mile = 1.85 km = 1.15 statute miles
1 fathom = 6 feet = 1.83 m
1 knot = 1 nautical mile per hour
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