The Saastamoinen model is a widely used empirical model in Global Navigation Satellite System (GNSS) processing.
Its primary purpose is to calculate and apply corrections for the delays that GNSS signals experience as they pass through the Earth's atmosphere, specifically the troposphere.
The model specifically calculates the zenith hydrostatic delay. This component represents the delay caused by atmospheric pressure and temperature under hydrostatic equilibrium conditions directly above the observer (at the zenith).
While the model can be extended to estimate the zenith wet delay, its core and most fundamental correction targets the hydrostatic component of the signal delay at the zenith.
Therefore, the Saastamoinen model provides a correction for zenith hydrostatic delay.
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?