GPS Tracking Device positioning is very accurate in the long term
Most of the error in GPS positioning comes from medium propagation effects that are unpredictable or difficult to model, including multipath (reflection of the signal before it finds the antenna) and tropospheric refraction. If one considers the basic error and operational characteristics of the INS, then a clear complementarity to GPS emerges. INS is very precise in the short term and yields data rates much higher than GPS. It is self-contained (Personal Tracker), except for initialization, and operates in any environment. On the other hand, GPS positioning is very accurate in the long term (drifts can be eliminated largely through data processing), it depends on a space segment that provides accurate orbit information, GPS data rates are only *noderatelyhigh, and the operational environment may limit the positioning capability. The integration of GPS and INS is the subject of Chapter 10; while, in the present chapter we review the essentials of obtaining observations with the Global Positioning System, aiming primarily at kinematic applications. It is beyond the present scope to expound in detail on the many aspects of the Global Positioning System including the broad range of applications,
There are several quantities that may be observed with a Waterproof GPS Tracker ; not all are routinely provided by every receiver. However, in one way or another, these observables are all connected to time, and time on board the satellite and in the receiver is kept by clocks that are, in fact, generators oscillating at a particular frequency. These oscillators are also responsible for generating the signals that are used to form the observables. But GPS is not without problems and limitations. In the first place, it is not a selfcontained, autonomous system like INS. The user must be able to "see" (in the sense of being able to receive transmitted signals from) the GPS satellites. Usually this is no problem, but satellite visibility may be obstructed locally by intervening buildings, foliage, mountains, bridges, and tunnels. This is because the carrier signal that the satellite transmits and that conveys positioning codes and the navigation message has a wavelength only 19 cm long (-1.6 GHz signal) and so will be severely attenuated even with light to moderate foliage and completely blocked by most larger structures. Certainly, direct underwater applications of GPS are completely impossible.
Although this signal shadowing is the most restrictive limitation, other problems
with Portable GPS Tracking prevent it from realizing the required accuracy and resolution in many kinematic applications. One of these arises from the effects of electronic interference or brief obstructions that may cause the receiver to miss one or more cycles of the carrier wave (this matters only if the carrier phase rather than the code is used for positioning). In fact, jamming and sustained electronic interference are general problems. The frequency of the data output in most receivers is often 1 Hz, rarely greater than 2 Hz without significant increase in the noise levels. This may not yield sufficient resolution or accuracy for airborne platforms that collect scientific data at a higher rate or at random intervals not precisely coincident with the GPS epochs.
More information at http://www.jimilab.com/ .