User Tools

Site Tools


start:hype_model_description:hype_tracer

Differences

This shows you the differences between two versions of the page.

Link to this comparison view

Both sides previous revision Previous revision
Next revision
Previous revision
Next revision Both sides next revision
start:hype_model_description:hype_tracer [2018/10/11 17:42]
cpers [Lake and river ice]
start:hype_model_description:hype_tracer [2018/10/11 17:43]
cpers [Lake and river ice]
Line 205: Line 205:
 <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. ​
Line 287: Line 287:
 |:::​|//​sndens//​|//​ricesndens,​ licesndens//​|:::​| |:::​|//​sndens//​|//​ricesndens,​ licesndens//​|:::​|
 |:::​|<​m>​p_m</​m>​|//​ricetmelt,​ licetmelt//​|:::​| |:::​|<​m>​p_m</​m>​|//​ricetmelt,​ licetmelt//​|:::​|
 +|:::​|//​meff//​|//​ricewme,​ licewme//​|:::​|
 |Surface water processes|//​tcf//​|//​tcfriver,​ tcflake//​|[[start:​hype_file_reference:​par.txt|par.txt]]| |Surface water processes|//​tcf//​|//​tcfriver,​ tcflake//​|[[start:​hype_file_reference:​par.txt|par.txt]]|
 |:::​|//​scf//​|//​scfriver,​ scflake//​|:::​| |:::​|//​scf//​|//​scfriver,​ scflake//​|:::​|
start/hype_model_description/hype_tracer.txt ยท Last modified: 2024/01/25 11:37 (external edit)