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start:hype_model_description:hype_tracer [2018/10/11 17:42] cpers [Links to file reference] |
start:hype_model_description:hype_tracer [2018/10/11 17:43] cpers [Lake and river ice] |
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<m> dH_i/dt=-p_m * T_a </m> | <m> dH_i/dt=-p_m * T_a </m> | ||
- | Ice can be melted from below if the water contain enough heat. This process is limited by a melt efficiency parameter (//me//). | + | Ice can be melted from below if the water contain enough heat. This process is limited by a melt efficiency parameter (//meff//). |
Final ice break-up is defined as the time step when //H<sub>i</sub>//=0. Although it is well known that ice tend to fall apart before it is completely melted, this is not considered by the present model. | Final ice break-up is defined as the time step when //H<sub>i</sub>//=0. Although it is well known that ice tend to fall apart before it is completely melted, this is not considered by the present model. |