Typhoon Melor was a weakening Category 2 typhoon on the morning of October 7, 2009, when the QuikSCAT satellite collected the observations used to make this image. The image depicts the wind field associated with the storm. The strongest winds are pink and purple, forming a rough circle in the center of the storm. Much of the rest of the storm is made up of a broad field of moderately strong winds, shown in red. Barbs illustrate wind direction, spiraling around the center of the storm. White barbs point to areas of heavy rain.
QuikSCAT collected these wind measurements at 5:35 a.m. (Tokyo time) on October 7 (20:35 UTC, October 6). At that time, Typhoon Melor had winds between 167 kilometers per hour (104 miles per hour or 90 knots) and 157 km/hr (98 mph or 85 knots), according to the Joint Typhoon Warning Center. The storm was moving towards Japan and was forecast to make landfall around 9:00 a.m. on October 8, local time.
QuikSCAT monitors wind speed with a radar that sends out pulses of
microwave energy and listens for the echo after the pulse bounces off
the wind-roughened ocean surface. Scientists translate radar signals
into estimates of wind speed by matching the radar echoes to physical
measurements collected from buoys at the same time and place.
Cyclone-strength wind speeds are rare, however, and scientists
generally don’t have enough matching buoy observations to
convert wind speeds above roughly 50 knots. Intense rain rippling the
ocean’s surface can also interfere with the radar signal.
Because of these limitations, QuikSCAT images don’t show
absolute, maximum wind speeds. Instead, they give forecasters a
valuable picture of the wind structure within the storm, for example,
revealing whether a storm has a strong or a weak eye and how large an
area is experiencing tropical-storm-strength winds.