PPS web services are now functioning normally. PPS has identified and fixed the previous production web server problem which caused the intermittent unavailability and/or slow response times experienced for the last few days. If you experience any further problems or inconsistencies with PPS web services including: ftp://arthurhou.pps.eosdis. nasa.gov ( GPM FTP data) http://pps. gsfc.nasa.gov (PPS home page) https://storm-pps.gsfc.nasa.gov (PPS STORM) http://registration.pps.eosdis.nasa.gov (PPS GPM registration) http://ceospc.gsfc.nasa.gov Once again, we sincerely appreciate everyone's

The GPM core observatory satellite continued to provide excellent coverage of Soudelor as the typhoon closed in on Taiwan. GPM flew directly above typhoon Soudelor's eye on August 7, 2015 at 1041Z (6:41 PM Local Time) when wind speeds were 110 kts (127 mph). Rainfall data from GPM's Microwave Imager (GMI) and Dual-Frequency Precipitation Radar (DPR) instruments revealed very heavy rainfall in spiraling bands rotating around a decaying inner eye wall. Precipitation intensity can be measured by the Dual-Frequency Precipitation Radar instrument mounted on the GPM core observatory satellite. Some

PPS web services are still experiencing intermittent unavailability and/or slow response times and our staff is working to resolve this problem as soon as possible. This problem impacts access to various PPS web services: ftp://arthurhou.pps.eosdis.nasa.gov (GPM FTP data) http://pps.gsfc.nasa.gov (PPS home page) https://storm-pps.gsfc.nasa.gov (PPS STORM) http://registration.pps.eosdis.nasa.gov (PPS GPM registration) http://ceospc.gsfc.nasa.gov GPM near real time operations and data distribution as well as PPS GPM operations are NOT affected. Only the PPS GPM data distribution is affected. We

Typhoon Soudelor's winds had dropped to 95 kts ( 109 mph) when the GPM core observatory satellite had another excellent daytime view on August 6, 2015 at 0006 UTC. GPM's Dual-Frequency Precipitation Radar (DPR) data showed that Soudelor had heavy rainfall in an inner eye wall and also in a much larger replacement outer eye wall. The heaviest rain found by GPM was dropping at a rate of close to 70 mm (2.4 inches) per hour in a strong feeder band spiraling in on the southwestern side of the typhoon. Radar reflectivity data from GPM's Dual-Frequency Precipitation Radar (DPR) data were also used

Typhoon Soudelor's sustained winds were about 105 kts ( about 121 mph) when the GPM core observatory satellite flew above on August 5, 2015 at 1051 UTC. A rainfall analysis was made from data collected from GPM's Microwave Imager (GMI) and Dual-Frequency Precipitation Radar (DPR) instruments. This analysis showed that Soudelor was very large and had a well defined eye. Intense feeder bands are shown spiraling into the center. Three dimensional radar reflectivity data GPM's DPR (ku Band) were used to construct a simulated cross section through typhoon Soudelor's center. This view from the south