[MITgcm-devel] seaice_budget_ice
Jinlun Zhang
zhang at apl.washington.edu
Wed Dec 27 13:01:55 EST 2006
Hi Martin,
Parkinson&Washington gives a very nice description about
surface_emissivity. It lists all the components of surface heat flux,
really an excellent paper about ice thermodynamics.
Jinlun
Martin Losch wrote:
> Thanks Jinlun,
> but then, what is the meaning of the of the term
> surface_emissivity*lwdown?
> (surface is both ice and ocean for the respective cases in budget) I
> would have thought that the radiation that is emitted by the surface
> is upward radiation, not downward. Or does one parameterize the
> emitted radiation as .97*lwdown?
>
> Martin
>
> On 27 Dec 2006, at 17:51, Jinlun Zhang wrote:
>
>> Hi Martin,
>> 0.97 is surface emissivity.
>> Jinlun
>>
>> Martin Losch wrote:
>>
>>> Hi Jinlun, Dimitris,
>>>
>>> Please forgive me, if I am confused about all these constants:
>>> I am currently trying to implement some radiation-bulk formulae
>>> that estimate lwdown from air and ocean temperature, humidity,
>>> because apparently for the Arctic the reanalysis fields for lwdown
>>> (and swdown) are not very good (this is what my Arctic specialists
>>> Gerdes, Karcher, Kauker, Koeberle tell me). The seaice-pkg has
>>> some remains of the original Parkinson&Washington bulk formulae in
>>> it, which is close to what we want to have for the Arctic (for
>>> comparison reasons), so I want to understand what the individual
>>> contributions are.
>>> So: What is the 0.97? ice emissivity? why then have .97*lwdown, if
>>> lwdown is not affected by the surface? Or is it some sort of
>>> albedo for long wave radiation? What variable name should I give
>>> to this number?
>>>
>>> Martin
>>>
>>> On 27 Dec 2006, at 07:23, Dimitris Menemenlis wrote:
>>>
>>>> Martin, why do you think that emissivity is already part of
>>>> lwdown? My understanding of the NCEP and ERA fields is that
>>>> lwdown and swdown are radiation fields prior to any interaction
>>>> with sea surface, as opposed to lwnet and swnet, which include
>>>> interaction with sea surface. A more serious issue is
>>>> potentially the lack of realism of the representation of
>>>> atmospheric boundary layer processes, especially in NCEP
>>>> reanalysis, which is the older of the two.
>>>>
>>>> A second comment is that by default we bypass the
>>>> seaice_budget_ocean bulk formulae and instead use that of pkg/exf.
>>>>
>>>> Dimitris
>>>>
>>>>> Whatever forcing one uses, make sure 0.97 is not used twice. Jinlun
>>>>> Martin Losch wrote:
>>>>>
>>>>>> Hi there,
>>>>>> why is lwdown (now lwdownLoc) mulitplied by 0.97 in
>>>>>> seaice_budget_ice
>>>>>> (formerly budget)? This looks awfully like some ocean surface
>>>>>> emissivity,
>>>>>> which is already part of lwdown if I am not mistaken. (the
>>>>>> same is true
>>>>>> for seaice_budget_ocean, also formerly budget.)
>>>>>> I think that this is wrong.
>>>>>> Martin
>>>>>
>>>>>
>>>> _______________________________________________
>>>> MITgcm-devel mailing list
>>>> MITgcm-devel at mitgcm.org
>>>> http://mitgcm.org/mailman/listinfo/mitgcm-devel
>>>
>>>
>>>
>>> _______________________________________________
>>> MITgcm-devel mailing list
>>> MITgcm-devel at mitgcm.org
>>> http://mitgcm.org/mailman/listinfo/mitgcm-devel
>>
More information about the MITgcm-devel
mailing list