Typhoon Chanchu is shown here as observed by NASA’s QuikSCAT satellite on May 10, 2005, at 21:11 UTC (which is May 11, 5:11 a.m. local time). At this time, the typhoon had sustained winds of 140 kilometers per hour (85 miles per hour; 75 knots). Chanchu crossed the threshold to typhoon status only a few hours after this image was captured.
The image shows wind speed in color and wind direction with small barbs. White barbs point to areas of heavy rain. The highest wind speeds, shown in purple, surround the center of the storm.
Other types of measurements of the wind strength of Typhoon Chanchu show sustained winds slightly higher than those shown by QuikSCAT observations. This difference is because the power of the storm makes accurate satellite measurements difficult. QuikSCAT’s scatterometer sends pulses of microwave energy through the atmosphere to the ocean surface, and measures the energy that bounces back from the wind-roughened surface. The energy of the microwave pulses changes depending on wind speed and direction, giving scientists a way to monitor wind around the world.
Tropical cyclones (the generic term for hurricanes and typhoons), however, are difficult to measure. To relate the radar signal observed by satellite to actual wind speed, scientists compare measurements taken from buoys and other ground stations to data the satellite acquired at the same time and place. Because the high wind speeds generated by cyclones are rare, scientists do not have corresponding ground information to know how to translate data from the satellite for wind speeds above 50 knots (about 93 km/hr or 58 mph). Also, the unusually heavy rain found in a cyclone distorts the microwave pulses in a number of ways, making a conversion to accurate wind speed difficult. Instead, the scatterometer provides a nice picture of the relative wind speeds within the storm and shows wind direction.
NASA image courtesy of David Long, Brigham Young University, on the QuikSCAT Science Team, and the Jet Propulsion Laboratory.
Tropical Storm Chanchu formed in the western Pacific on May 8, 2006, roughly 500 miles east of the Philippines. The storm has been gradually building strength and size, and was upgraded to typhoon status late on May 10.