For user channels, we employ the Gilbert Elliot model with a flow-level interpretation: the channel condition follows a general two-state Markov chain with distinct probabilities of finishing the flow transmission.
2. Interpretation Tributary channels and major channels within LMVs have similar sedimentary characteristics but can be distinguished based on the following aspects: major channels developed within long, wide, confined areas, which result in low-frequency lateral accretion but high-frequency vertical accretion.
With this interpretation, the channel access can again be done exclusively, but each subcarrier might be shared over time.
In fact, without information of the other channels, there are several interpretations for channel 30 according to ACF.
It is our interpretation that the channel heads that did not initiate at groundwater seeps were affected by human disturbance (forest conversion for swidden-based agriculture), as they tend to lay above seeps on highly disturbed hillslopes.
Detailed interpretation of single channel seismic reflection and Huntec deep-tow boomer and sparker profiles demonstrates that the southwestern Black Sea shelf formed by a protracted shelf-edge progradation since the Miocene Pliocene.
The mechanism(s) that have been developed will be important in the interpretation of ion channel data and the predicted changes in the action potential using suggested in silico models.
Since more is known about the BK channels, we focused our study design and interpretation on these channels (see schematic in Figure 1b).
