- 2
- Campaigns
- 0
- Data Products


Overview
The NASA SIERRA is an uncrewed aircraft system designed by the U.S. Naval Research Laboratory. It is well-suited for atmospheric and remote sensing research missions in isolated regions such as the Arctic, where it is more dangerous for other aircraft to fly. The SIERRA can carry payloads up to 110 lbs. and reach a maximum altitude of 13,000 ft. allowing for more accurate data collection.
Related Campaigns & Instruments
Review the instruments operated on this platform for each of these field campaigns
Slide 1 of 2

Characterization of Arctic Sea Ice Experiment
2009
Svalbard archipelago of Norway
view all deployment dates
1 Deployment
· 0 Data Products2009-07-13 | 2009-07-29 |
Generic-Atmospheric State (Gen-AtmsState) refers to non-specific instruments on a platform used for measurements of atmospheric state parameters. These are typically in situ sensors that measure temperature, pressure, humidity, and wind speed/direction. Types of atmospheric state instruments include thermometers, hygrometers, barometers, and anemometers.
Earth Science > Atmosphere > Atmospheric Water Vapor
Earth Science > Atmosphere > Atmospheric Pressure
Earth Science > Atmosphere > Atmospheric Water Vapor > Water Vapor Indicators > Humidity
Earth Science > Atmosphere > Atmospheric Temperature > Surface Temperature > Air Temperature
Earth Science > Atmosphere > Atmospheric Winds > Upper Level Winds > Wind Direction
Earth Science > Atmosphere > Atmospheric Winds > Upper Level Winds > Wind Speed
Earth Science > Atmosphere > Atmospheric Pressure > Atmospheric Pressure Measurements
Earth Science > Atmosphere > Atmospheric Winds > Surface Winds > Wind Direction
Earth Science > Atmosphere > Atmospheric Temperature
Earth Science > Atmosphere > Atmospheric Winds > Surface Winds > Wind Speed
Earth Science > Atmosphere > Atmospheric Winds
The Micro Advanced Synthetic Aperture Radar (MicroASAR) is an airborne radar system developed by Brigham Young University (BYU) and Artemis, Inc. It was designed to operate on uncrewed aerial systems (UAS) and small aircraft. It is a C-band (5428.76 MHz) synthetic aperture radar (SAR) that provides radar imagery at a nominal range resolution of 1 m at a 160 MHz bandwidth. MicroASAR can operate at altitudes ranging from 500 to 3000 ft and has a maximum swath width of 300 to 2500 m.
Earth Science > Spectral/engineering > Radar
Earth Science > Spectral/engineering > Radar > Radar Imagery
A pyrometer is a remote-sensing infrared thermometer that measures the temperature of distant objects. It determines the temperature of an object by detecting its thermal radiation. It can be deployed on aircraft, ground, or water-based platforms for surface and sea surface temperature observations. For atmospheric studies, the pyrometer typically operates in the 9.6 to 11.5 µm spectral range and has a temperature range of -25 to 200 degrees Celsius. Pyrometers have a typical response time of 5 ms to 600 s.
Earth Science > Oceans > Ocean Temperature > Sea Surface Temperature
Earth Science > Atmosphere > Atmospheric Temperature > Surface Temperature > Skin Temperature
Earth Science > Atmosphere > Atmospheric Temperature > Surface Temperature
Earth Science > Spectral/engineering > Infrared Wavelengths > Brightness Temperature
The CU LIDAR Profilometer and Imaging System (CULPIS) is an airborne lidar mapping system developed at the University of Colorado at Boulder. It is designed to map land and sea ice surface topography and elevation from uncrewed aerial systems (UAS). It consists of a lidar system, an inertial measurement unit (IMU), a global positioning system (GPS), and digital cameras. The lidar system within CULPIS operates at the 905 nm wavelength and has a measurement rate of 400 Hz. It has a lidar footprint of 60 cm and an along-track spacing of 7.5 cm at a flight altitude of 200 m above ground level (AGL) and a flight speed of 30 meters per second.
Earth Science > Terrestrial Hydrosphere > Glaciers/ice Sheets > Glacier Topography/ice Sheet Topography
Earth Science > Land Surface > Topography > Terrain Elevation
Earth Science > Cryosphere > Glaciers/ice Sheets > Glacier Topography/ice Sheet Topography
Earth Science > Spectral/engineering > Lidar
Earth Science > Oceans > Sea Ice > Sea Ice Elevation
Earth Science > Land Surface > Topography
Earth Science > Cryosphere > Sea Ice > Sea Ice Elevation
If instrument mode or detailed specification information is not available, can use this entry for spectrometers of various types. A spectrometer is an instrument that measures a range of a characteristic for a given substance or wavelength. There are many different types of spectrometers. Some examples are mass spectrometers, spectrophotometers, and magnetic radiation spectrometers.
Earth Science > Spectral/engineering > Infrared Wavelengths
Earth Science > Spectral/engineering > Ultraviolet Wavelengths
Digital cameras are used to provide imagery for research applications. Cameras are used on aircraft to collect aerial imagery for mapping and surveying, environmental monitoring, cloud observations, agriculture, geological studies, and other Earth science applications. They are also used at field sites to capture visual observations to monitor changes in land cover, vegetation, clouds, air quality, glaciers, and other phenomena.
Earth Science > Spectral/engineering > Visible Wavelengths > Visible Imagery

Marginal Ice Zone Ocean and Ice Observations and Processes Experiment
2013
Southern Beaufort Sea, Prudhoe Bay, Alaska
view all deployment dates
1 Deployment
· 0 Data Products2013-07-09 | 2013-08-09 |
This data will be added in future versions.
Earth Science > >
A pyrometer is a remote-sensing infrared thermometer that measures the temperature of distant objects. It determines the temperature of an object by detecting its thermal radiation. It can be deployed on aircraft, ground, or water-based platforms for surface and sea surface temperature observations. For atmospheric studies, the pyrometer typically operates in the 9.6 to 11.5 µm spectral range and has a temperature range of -25 to 200 degrees Celsius. Pyrometers have a typical response time of 5 ms to 600 s.
Earth Science > Oceans > Ocean Temperature > Sea Surface Temperature
Earth Science > Atmosphere > Atmospheric Temperature > Surface Temperature > Skin Temperature
Earth Science > Atmosphere > Atmospheric Temperature > Surface Temperature
Earth Science > Spectral/engineering > Infrared Wavelengths > Brightness Temperature
The CU LIDAR Profilometer and Imaging System (CULPIS) is an airborne lidar mapping system developed at the University of Colorado at Boulder. It is designed to map land and sea ice surface topography and elevation from uncrewed aerial systems (UAS). It consists of a lidar system, an inertial measurement unit (IMU), a global positioning system (GPS), and digital cameras. The lidar system within CULPIS operates at the 905 nm wavelength and has a measurement rate of 400 Hz. It has a lidar footprint of 60 cm and an along-track spacing of 7.5 cm at a flight altitude of 200 m above ground level (AGL) and a flight speed of 30 meters per second.
Earth Science > Terrestrial Hydrosphere > Glaciers/ice Sheets > Glacier Topography/ice Sheet Topography
Earth Science > Land Surface > Topography > Terrain Elevation
Earth Science > Cryosphere > Glaciers/ice Sheets > Glacier Topography/ice Sheet Topography
Earth Science > Spectral/engineering > Lidar
Earth Science > Oceans > Sea Ice > Sea Ice Elevation
Earth Science > Land Surface > Topography
Earth Science > Cryosphere > Sea Ice > Sea Ice Elevation
This data will be added in future versions
Earth Science > Atmosphere > Atmospheric Radiation
This data will be added in future versions.
Earth Science > >
Digital cameras are used to provide imagery for research applications. Cameras are used on aircraft to collect aerial imagery for mapping and surveying, environmental monitoring, cloud observations, agriculture, geological studies, and other Earth science applications. They are also used at field sites to capture visual observations to monitor changes in land cover, vegetation, clouds, air quality, glaciers, and other phenomena.
Earth Science > Spectral/engineering > Visible Wavelengths > Visible Imagery
The Ball Experimental Sea Surface Temperature Radiometer (BESST) is an airborne pushbroom imaging radiometer developed by Ball Aerospace. It is a thermal infrared (8-12 μm) radiometer that measures sea surface temperature. BESST has a spatial resolution of 1 meter and a swath width of 200 meters at a flight altitude of 600 meters. It collects a total of 130 frames during a data frame, which takes about 53 seconds to complete. BESST was designed to be deployed on uncrewed aerial systems (UAS) and small aircraft.
Earth Science > Oceans > Ocean Temperature > Sea Surface Temperature
Earth Science > Spectral/engineering > Infrared Wavelengths > Thermal Infrared
The Digital Mapping System (DMS) is an airborne camera system maintained and operated by the Airborne Sensor Facility (ASF) located at NASA Ames Research Center (ARC). It captures high resolution natural color and panchromatic images of terrain which can be used to create mosaics and topographic maps. DMS has a cross-track spatial resolution of 10 cm at nadir and swath width of about 570 m at a flight altitude of 1,500 feet. The DMS is ideal for a variety of scientific programs to monitor variation in environmental conditions, assess global change, and respond to natural disasters
Earth Science > Spectral/engineering > Visible Wavelengths > Visible Imagery
If instrument mode or detailed specification information is not available, can use this entry for spectrometers of various types. A spectrometer is an instrument that measures a range of a characteristic for a given substance or wavelength. There are many different types of spectrometers. Some examples are mass spectrometers, spectrophotometers, and magnetic radiation spectrometers.
Earth Science > Spectral/engineering > Infrared Wavelengths
Earth Science > Spectral/engineering > Ultraviolet Wavelengths
Lidar is a surveying method that measures distance to a target by illuminating the target with laser light and measuring the reflected light with a sensor. Differences in laser return times and wavelengths can then be used to make digital 3-D representations of the target.
Earth Science > >
This data will be added in future versions.
Earth Science > >
This data will be added in future versions.
Earth Science > >