In Global Navigation Satellite System (GNSS) positioning, particularly when using carrier phase measurements for high precision, cycle slips represent a sudden jump in the observed phase by an integer number of cycles.
Cycle slips are most detrimental for estimating integer ambiguity. Here's why:
While cycle slips can indirectly affect other estimations, their primary impact is on integer ambiguity resolution:
Therefore, the accurate estimation of integer ambiguity is critically dependent on the absence or proper detection and correction of cycle slips in GNSS carrier phase measurements.
The carrier phase observation model in GNSS is given as $$ \phi_A^i = f \delta^i - \frac{\rho_A^i}{\lambda} - f \delta_A + N_A^i - f \delta_{\text{iono}} + f \delta_{\text{tropo}} + \epsilon $$ where $\phi_A^i$ is the observed carrier phase in cycles, $f$ is the frequency of the carrier in hertz, and $\lambda$ is the wavelength of the carrier in meters.
What is the unit of the ionospheric ($\delta_{\text{iono}}$) and tropospheric ($\delta_{\text{tropo}}$) delay terms in the given equation?