Monthly Archives: May 2011

NASA G-III Completes Successful Flights in Hawaii

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The NASA Gulfstream-III aircraft returned to Palmdale, Calif., onTuesday May 10, 2011 from a successful nine-day mission to the Big Island ofHawaii.  The goal of the missionwas to image volcanoes on the Big Island and map surface deformations on Oahu,Molokai, and Maui using an airborne radar system installed in the G-III calledthe Uninhabited Aerial Vehicle Synthetic ApertureRadar (UAVSAR).  


G-III flight crew and scientists on May 2, 2011 at Kona International Airport (Image Credit: Bradley Pacific Aviation)


Seven science flights totaling 39.3 hours were flown overthe nine-day deployment.  “These repeat data acquisitions will allow us to image thesurface displacement from the March 2011 Kilauea fissure eruption along itseast rift zone at unprecedented resolution” said Paul Lundgren, NASA JetPropulsion Laboratory research scientist and principal investigator of thevolcano study.  Future plans are to return to Hawaii at roughly year-longintervals (or sooner if new significant eruptive activity occurs). UAVSARprovides unique data than can improve our understanding of eruption source processes.   The data collected on thismission will provide a basis for comparison with future missions flown inresponse to new or impending volcanic eruptions.


The G-III flies at 41,000 ft to collect airborne radar data.  A break in the clouds allowed Tim Moes onboard the G-III to take this image of the snow-covered summit of Mauna Kea (14,000 ft) with its many astronomical observatories

Broadband Lidar Instrument Team Concludes Successful Test Flights on the NASA DC-8

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How do instruments end up on satellites orbiting the Earth? 

For many of them, long before they are ever launched into space, they are tested from NASA airplanes. One of the objectives of the NASA Airborne Science Program is to test new instruments in space-like environments. Testing future satellite instruments from airplanes is the next best thing to actually testing them in space.


The NASA DC-8 at the Dryden Aircraft Operations Facility in Palmdale, CA (Credit: E. Schaller)

Over the past three weeks, a team from the Goddard Space Flight Center led by Bill Heaps has been testing an instrument on the NASA DC-8 that they hope will fly on the ASCENDS satellite mission. ASCENDS (Active Sensing of Carbon dioxide Emissions over Nights Days and Seasons) is an upcoming NASA satellite expected to be launched in 2018-2020. The goal of ASCENDS is to measure the sources, distribution, and variations in carbon dioxide gas to a very high precision all over the Earth. Mapping carbon dioxide is important for understanding the global carbon cycle and for modeling global climate change.


Bill Heaps tests the Broadband Lidar instrument inside the NASA DC-8 (Image Credit:  E. Georgieva)

How do you measure carbon dioxide from space? Carbon dioxide makes up a very small fraction of the gas in Earth’s atmosphere. In addition, the majority of the carbon dioxide variability occurs in the first hundred feet above the surface of the Earth. In order to measure the abundance of carbon dioxide from a satellite, any instrument must therefore look through Earth’s entire atmosphere in order to detect the variations in carbon dioxide occurring near the surface.

Heaps’ instrument, a broadband Lidar, uses an infrared laser beam aimed at the surface of the Earth.  As the laser passes through the atmosphere and bounces off of the ground, carbon dioxide molecules in the atmosphere absorb some of the light from the laser.  Measuring the amount of absorption that occurs as the instrument passes over different locations on the Earth will allow the team to build global carbon dioxide maps.


Typical Lidar systems have lasers that emit light at very specific colors (wavelengths). The broadband laser used in Heaps’ instrument emits light with a broader range of wavelengths. The carbon dioxide molecule absorbs light at a several different infrared wavelengths. A broadband Lidar, therefore, has the advantage of being able to detect carbon dioxide absorption in multiple wavelength bands with one laser. The wavelength control requirements are also less strict than for a more conventional narrowband laser, which may make the system easier to implement on a satellite.

The Goddard team worked for over two weeks to install and test their instrument on the DC-8 on the ground at the NASA Dryden Aircraft Operations Facility in Palmdale, California. 


Broadband Lidar Instrument team members (Wen Huang and Elena Georgieva) test the performance of their laser inside the DC-8 at the NASA Dryden Aircraft Operations Facility (Image Credit:  W. Heaps)


This week, the team flew with their instrument on two, four-hour flights on the DC-8. During the flights, they tested the instrument performance at variety of altitudes and over different types of surfaces (deserts, agricultural fields, mountainous terrain, the ocean, and the flat waters of Lake Tahoe). The team was very pleased with the performance of the instrument. “The system definitely measured CO2 on both flights even transmitting a very small amount of laser power. I believe the broadband technique has excellent potential to be scaled up for measurements from space,” Heaps said.


DC-8 flight track (in red) from Wednesday May 4, 2011.  During the four-hour flight, the Broadband Lidar Instrument was tested at variety of altitudes and over a variety of different surface terrains.


This July, several instrument teams all vying to be chosen to fly on ASCENDS will test their instruments side by side on the DC-8. With data from the test flights of the Broadband Lidar Instrument in hand, Heaps’ team will return to Goddard to make refinements and improvements in the hope that their instrument will be chosen to fly on the ASCENDS satellite mission.

Funding for the Goddard Broadband Lidar was provided by the NASA Earth Science Technology Office Instrument Incubator program.