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The current population is equal to the the population of the previous generation multiplied by the rate of increase, multiplied by the carrying capacity minus the population of the previous generation divided by the carrying capacity, plus the current population.
This activity has enabled us to model different scenarios on different populations. Rather than spending massive amounts of time trying to figure out the effect of certain factors when they change, with the formulas in the spreadsheets, just by changing the number, all results will change with it as well. This helps us with a visual representation of what’s going on and what is being affected, as well as saving us time. Within science, several changes occur, whether they are expected or not. Being that there are so many changes, modeling scenarios in this manner help us express the changes better and in a short period of time.
1 comment:
It's interesting. Why do you think N doesn't just slope down to the new K after the drought?
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