GRAA NEWSLETTER
P.O. Box 1184, Greenbelt, MD 20768-1184
April 2018 | http://graa.gsfc.nasa.gov | 34th Year of Publication |
IMPORTANT DATES
April 10 | Mark your calendar for the GRAA Luncheon starting at 11:15 a.m. at the Greenbelt American Legion Post #136 at 6900 Greenbelt Road. Reservations are required, so please contact Alberta Moran on her cell phone at 301-910-0177 or via her email address at bertiemae90@gmail.com not later than noon on April 6th. The luncheon program will be the 35th Anniversary to commemorate the Tracking & Data Relay Satellite System (TDRSS) and the launch of TDRS-1. David Littmann, current TDRS Project Manager, will outline the history of the TDRSS Program, with pioneer Edmund Habib and previous project managers Anthony Comberiate, Ronald Browning, and perhaps others who managed TDRS-related matters since TDRS was conceived in '70s, may address key events during development, operations, and even the tragic loss of TDRS-2 when Challenger exploded in 1986. |
May 8 | Mark your calendar for the GRAA Luncheon starting at 11:15 a.m. Our speaker will be Dr. Stephen Volz, Assistant Administrator for Satellite and Information Services of the National Oceanic and Atmospheric Administration. The title/subject of his presentation will likely appear in the May newsletter. |
COMMENTS FROM TONY COMBERIATE, GRAA PRESIDENT: Our March speaker was Dr. James Abshire, Goddard Senior Scientist for Laser Sensing in the Solar System Exploration Division of the Sciences and Exploration Directorate and a pioneer in laser sensing from space. His talk, entitled "NASA Goddard's Space Lidar Measurements of the Earth and Planets," traced the results and evolution of laser measurements in space over the last five decades. Jim explained the difference between lasers and lidar. Lasers use stimulated emissions to generate light, collimated into a very fine beam, which is coherent in both time and space. LIDAR (light detection and ranging) is a surveying method that measures distances using laser technology similar to radar for radio frequencies. The first use of lasers at Goddard was to optically track spacecraft for orbit determination. Lidars were subsequently put on satellites to accurately map the topography of the surface below them. By 1971, laser altimeters were being used in the Apollo program to measure the shape of the moon and the height of its craters. Almost 20 years later, the MOLA instrument on the Mars Observer spacecraft very accurately mapped the entire planet (600 million measurements) from a 400 km polar orbit. Lasers had evolved significantly in both pulse rate (10/sec vs. 1 every 20 sec) and lifetime (~1 billion vs. 1 million).
In 1996-1997, Goddard flew augmented spare parts of the MOLA system in two Getaway special cans on the Space Shuttle to simultaneously observe both the tree canopy and the ground to determine tree height and to do vegetation mapping. A Geoscience Laser Altimeter System (GLAS) was later used by Goddard's ICEsat spacecraft (2003-2009) to measure the height of the Greenland and Antarctic ice sheets and to determine how they changed over time. Ice sheets were found to be thickening in the continental center from increased snowfall while thinning at the edges due to warming. It was also noticed that the elevation over the sub-glacial lakes was changing as if the lakes were interconnected.
In 2011, the laser altimeter on the Messenger orbit around the planet Mercury found permanently shadowed north polar craters that remain very cold despite their proximity to the Sun, perhaps retaining water. The Lunar Reconnaissance Orbiter is now mapping the Moon's surface in tremendous detail using five simultaneous beams from a 50 km orbit. It has also found permanently shadowed regions where ice could be trapped.
In 2018, new missions include ICEsat 2 that will use six beams to do more accurate mappings of ice sheets. The Global Ecosystem Dynamics Investigation (GEDI) mission will be launched in 2019 to measure Earth's ecosystems (+/- 50 degrees latitude) from the International Space Station. Dr. Abshire closed by emphasizing the dramatic process in the precise mapping of Earth and other planets that he has experienced in his career and thanked his colleagues for the opportunity to work at such an awesome place like Goddard for over four decades and he looks forward to mapping icy planets like Europa in the future.
TREASURER'S REPORT: Treasurer Jackie Gasch received tax-deductible donations from: Glenn Harris, Patricia Hensel, David Manges, Raymond Mazur, Christopher Scherer, and Charles Woodyard.
THOUGHT FOR APRIL: We really start aging more quickly once we finally realize we get the same sensation from a rocking chair that we once got from a roller coaster!
FROM THE GODDARD ARCHIVES – IT HAPPENED IN APRIL: Constructed by TRW, TDRS-1 was launched on the maiden flight of Space Shuttle Challenger from Cape Canaveral, FL, at 18:30 UTC on April 4, 1983. While at the pad, issues were detected with the Challenger's main engines and repairs were begun. At the time, a severe storm caused contamination of TDRS-1, so the satellite was cleaned and launched at the time stated above. Following deployment, TDRS-1 was to be raised to its operational geosynchronous orbit by means of an Inertial Upper Stage (IUS), which consisted of two solid rocket motors - the first used to raise the orbit's apogee and the second its perigee. The first burn was successful, but the IUS went out of control during the second burn. TDRS-1 separated from the upper stage in a lower than planned orbit but was raised to geosynchronous orbit by means of its attitude control system. Initially designed for seven years, TDRS-1 was moved to a decommissioning orbit after the last functioning traveling-wave amplifier failed in October 2009, rendering it unusable for communications purposes. Decommissioning was complete on June 27, 2010.
REMEMBERING OUR FORMER COLLEAGUES: