SMAP is a remote sensing observatory that carries two instruments that will map soil moisture and determine the freeze or thaw state of the same area being mapped. Soil moisture content is mapped via a combination of radar and radiometer measurements, while the freeze/thaw mapping is accomplished using unique properties of the radar system’s measurements. Both the radar and radiometer share a common antenna and feed assembly externally, but their electronics inside SMAP are different. When combined, the SMAP radar and radiometer will deliver high accuracy, high resolution global maps of the Earth’s soil moisture and freeze/thaw state.

Observatory-Vertical
The radar sends pulses of radio waves down to a spot on Earth and measures the echo that returns a few microseconds later. The strength and “shape” of the echoes can be interpreted to indicate the moisture level of the soil, even through moderate levels of vegetation. Since the radar actively sends and receives radio waves, this is where the ‘active’ in SMAP comes from.

The radiometer detects radio waves that are emitted by the ground from the same small area. The strength of the emission is an indicator of the temperature of the ground in that location. Since a radiometer passively makes these temperature measurements, this is where the ‘passive’ in SMAP comes from.

The large antenna that is shared by both radar and radiometer is SMAP’s most prominent feature. It operates just like a satellite dish, only is much larger, where a reflector collects all of the radio waves which focuses them into the feedhorn. Like a funnel, the feedhorn collects the echoes from the radar and the surface emissions from the radiometer and sends them to the radar and radiometer electronics for processing images. The feedhorn is a large cone visible on the outside of the spacecraft. The antenna reflector is a mesh antenna 6 meters (about 20 feet) in diameter.  

SMAP-Antenna
In order to achieve large coverage on the ground the antenna spins at 14.6 revolutions per minute (one revolution every 4 seconds). SMAP’s orbital motion combined with the spin of the antenna sweeps a small field of view in a series of overlapping loops that create a swath 1000 km (621 miles) wide. This large swath coverage allows SMAP to make complete soil moisture maps of the Earth repeated every 2 to 3 days. Soil moisture maps will be spaced at 10 km (6.2 miles), while freeze/thaw maps can distinguish areas as small as 3 km (1.9 miles).  

SMAP’s orbit is 685 km (426 miles) above Earth’s surface. Because Earth spins while SMAP orbits, swaths from each orbit are offset from each other and, after 8 days, the same swath is repeated. Over 2 to 3 days (2 days at the poles and 3 days at the equator), the gaps between swaths are filled in and a global map of moisture and frozen land can be prepared. Data taken by SMAP’s two instruments run from pole to pole. The orbit is oriented such that it crosses Earth’s terminator at the equator.  (The terminator is the boundary between day and night, either at sunrise or at sunset.)  

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