When an interplanetary vehicle arrives at its destination, it must reduce its
velocity to achieve orbit or to land. To reach a low, near-
circular orbit around a body with substantial
gravity (as is required for many scientific studies), the required velocity changes can be on the order of kilometers per second. Using propulsion, the
rocket equation dictates that a large fraction of the spacecraft mass must consist of fuel. This reduces the science payload and/or requires a large and expensive rocket. Provided the target body has an atmosphere, aerobraking can be used to reduce fuel requirements. The use of a relatively small burn allows the spacecraft to enter an elongated
elliptic orbit. Aerobraking then shortens the orbit into a circle. If the atmosphere is thick enough, a single pass can be sufficient to adjust the orbit. However, aerobraking typically requires multiple orbits higher in the atmosphere. This reduces the effects of
frictional heating, unpredictable turbulence effects, atmospheric composition, and temperature. Aerobraking done this way allows sufficient time after each pass to measure the velocity change and make corrections for the next pass. Achieving the final orbit may take over six
months for
Mars, and may require hundreds of passes through the atmosphere. After the last pass, if the spacecraft is to stay in orbit, it must be given more
kinetic energy via rocket engines in order to raise the
periapsis above the atmosphere. If the craft is to land, it must lose kinetic energy, also via rocket engines. The kinetic energy
dissipated by aerobraking is converted to
heat, meaning that spacecraft must dissipate this heat. The spacecraft must have sufficient surface area and structural strength to produce and survive the required drag. The temperatures and pressures associated with aerobraking are not as severe as those of
atmospheric reentry or
aerocapture. Simulations of the
Mars Reconnaissance Orbiter aerobraking use a
force limit of 0.35
N per square meter with a spacecraft cross section of about 37 m2, equate to a maximum drag force of about 7.4 N, and a maximum expected
temperature as 170 °C. The force density (i.e. pressure), roughly 0.2 N per square meter, that was exerted on the
Mars Observer during aerobraking is comparable to the aerodynamic resistance of moving at 0.6 m/s (2.16 km/h) at sea level on Earth, approximately the amount experienced when walking slowly. Regarding spacecraft navigation,
Moriba Jah was the first to demonstrate the ability to process Inertial Measurement Unit (IMU) data collected on board the spacecraft, during aerobraking, using an unscented
Kalman Filter to statistically infer the spacecraft's trajectory independent of ground-based measurement data. Jah did this using actual IMU data from
Mars Odyssey and
Mars Reconnaissance Orbiter. Moreover, this was the first use of an unscented
Kalman Filter to determine the orbit of an anthropogenic space object about another planet. This method, which could be used to automate aerobraking navigation, is called Inertial Measurements for Aeroassisted Navigation (IMAN) and Jah won a
NASA Space Act Award for this work. Many spacecraft use solar panels to power their operations. The panels can be used to refine aerobraking to reduce the number of required orbits. The panels rotate according to an AI-powered algorithm to increase/reduce drag and can reduce arrival times from months to weeks. ==Related methods==