NOAA satellite images for SSO observers
The images received from the low-earth-orbit NOAA satellites
are similar to those from the Japanese geostationary satellite, GMS-5.
GMS-5 is the source of most Australian weather sat imagery, such
as that
presented on TV, and on the Bureau of
Met , James
Cook Uni satellite image web sites. There are other NOAA
receiving stations in Australia, but images presented on this web site
are generated by a seriously clever computer program known as WXtoImg, and are
different from GMS-5 images in a few key ways:
- Higher resolution - pixel size = 4km.
- A convenient symbol (
+ ) drawn on images, indicating
the whereabouts of SSO.
-
WXtoImg-generated images are
actually overlaid composite images formed from
image pairs taken in two IR bands (daytime: near-
& thermal-IR, nighttime: mid- & thermal-IR). During
processing, natural looking land & sea colours are overlaid onto
the images. Daytime
MSA nighttime
MCIR enhanced images are coloured to look superficially similar.
Daytime
MSA images (near- & mid-IR composites) are impressive at showing
cloud and vegetation forms, especially when the sun is at low
elevation. Pre-twilight passes are usually very good at showing
any low cloud in the local area.
Cloud on the
images is normally coloured white, except when the cloud-top
temperature is < -20C, in which case it is coloured
green. Such coloured cloud is normally associated with rain, and
approaching rain-bearing fronts and troughs are clearly depicted.
For interest, yellow cloud has cloud-top temperatures < -30C,
red < -40C, and for
black cloud... take cover!
With a knowledge of
the satellite pass schedule, near real-time images are periodically
available to an observer. A satellite pass
takes ~10-15minutes to complete, and image processing and transfer of
images to the web site takes ~5 minutes. Such near-real-time
data, combined
with an accurately placed map overlay, mean that an observer can
usually
relate current out-the-window cloud observations with those on the
satellite
image, and can often take an informed punt on local cloud motion and
structure. Also one can estimate the passage and size of cloud
bands, and of the
larger 'sucker
holes'.
- Our web page presents the last couple of days of images, in a
sequence of thumbprint images. These provide a quick visual
reference of the development and approach of large scale cloud patterns.
- Raw images are transformed to a polar stereographic projection,
and
presented on a standard map, bounded approximately by Longitudes 130°
&160° East,
and Latitudes 20° & 45° South.
As with the IR images produced from GMS-5, clouds are easiest to spot
when at higher altitudes, when they are cold relative to the ground.
Low level cloud does not show up well on the nighttime MCIR
images.
The NOAA satellites orbit at just over 800km altitude, and along their
orbital track they scan a swath of Earth about 2800km wide.
Many orbital passes received at SSO are so distant that SSO is
left
off-the-map, but images posted on these web pages are selected so that
SSO always appears on the image, even if at an extreme edge.
At present there are four active NOAA satellites generating images
displayed at this site, namely NOAAs 12, 15, 17 and 18. All four
are
in sun-synchronous polar orbits, meaning that the planes of their
orbits remain approximately the same relative to that of the Earth's
day/night terminator. As the Earth rotates, SSO passes through
the plane
of NOAA-12's orbit at 4:24am, and again 12.9 hours later at 5:19pm.
Likewise
for NOAAs 15, 17, and 18, passage through the orbital planes will occur
at 5:21am/18:15pm, 9:52am/10:46pm, and 1:14am/2:12pm respectively.
So an SSO observer will see NOAA
passes
centred on the times 01:15,
04:24, 05:21, 9:52, 14:12, 17:19, 18:15 and
22:46 AEST.
1-2
passes of a NOAA satellite will occur within ±1 hour of these times.
The present receiving antenna, located approximately 50m uphill of the
APT building, is known as a Lindenblad
type. It is designed for the reception of the
right-hand-circularly-polarised (RHCP) radio waves transmitted by NOAA
satellites, a job it does superbly. But its one big drawback is a
reception 'dead zone' located toward the zenith. Occasionally
high-elevation satellite passes (with a maximum elevation ~ >80°)
pass though this 'cone-of-silence', and a 'salt-and-pepper' pattern of
interference appears across the image, usually passing right though the
location of SSO. Since SSO observers are particulary interested
in local cloud conditions, this interference
stripe is particularly inconvenient. Consequently, during April
2004 I reoriented
the receiving antenna to make it more sensitive to satellite
signals from near the zenith. This means that the image quality
is now likely to be poorer over Tasmania and Queensland, but locally to
SSO it's now pretty good. On rare occasions, interfering
radio signals from junk satellites may place noise stripes across
otherwise good images.
A thumbnail
image of today's latest downloaded image is shown at the left, and it
has a generic URL of
http://www.phys.unsw.edu.au/~map/weather/latest-thumb.jpg . One
application of this thumbnail, for webpage designers, is as an
attractive link to our main satellite image page. For example,
latest-thumb.jpg icons
are a feature of the AAO
weather
page, and the Coonabarabran.com.
Just for fun, occasionally I like to check who's
linked to our homepage.
For comments and suggestions concerning these web pages, please contact
Andre
at the
UNSW Automated Patrol Telescope
Siding Spring Observatory
Coonabarabran, NSW 2357
2005-06-07