Hi Steve,
I heard that present version of lake model works only in serial mode. What about latest version which you are going to
put in the latest version of RegCM3. Does that works also in Parallel mode?
Regards
Imran Nadeem
On 6/28/07, Richard Anyah <anyah@cep.rutgers.edu> wrote:
Steve,
That would be great. Update us when you get time to do it.
Thanks
Richard
Steve Hostetler wrote:
> Richard,
> I have a newer version of the lake model. I am plan to put it into
> the newest version of RegCM when I can find the time-- maybe sometime
> this fall.
>
> steve
>
>-----------------------------------------------------
>Steve Hostetler
>US Geological Survey
>Department of Geosciences
>Room 104 Wilikinson Hall
>Oregon State University
>Corvallis, OR 97331-5560
>tel 541 737-8928 fax 541 737-1200
>
>
>
>
> Richard Anyah wrote:
>
>>Hi Mike,
>>When the lake is turned off, the lake surface is treated as inland water
>>body(patch) in the land surface scheme(BATS). In which case, the fluxes
>>over the water patch may be different from the rest of the land cells.
>>But, when you use the 1D lake, you introduce the vertical flux transport
>>within the water column(full depth) and to the atmosphere which mayl
>>signficantly change the atmospheric response; depending on the size and
>>depth of the lake.
>>
>>
>>The reference below may be useful. They used one of the original
>>versions of RegCM. The lake model has not changed so much, I think. You
>>could also check Hostetler et al., 1993 (check details in the ref. below).
>>
>>*
>>*Gary T. Bates, Steven W. Hostetler, and Filippo Giorgi, 1995: Two-Year
>>Simulation of the Great Lakes Region with a Coupled Modeling System.
>>Monthly Weather Review:123, 1505 1522
>> Richard
>>
>>
>>Michael Notaro wrote:
>>
>>
>>
>>>Thanks, Richard! You have been quite helpful. I will look at those
>>>papers.
>>>
>>>I want to clarify one thing.
>>>When the lake is "turned off" then, does that mean the the lake does
>>>not exist
>>>and it is treated as land (bare soil, forest?)? So, if I run with
>>>and without the lake model,
>>>the difference is the effect of the existence of those lakes on the
>>>atmosphere? I was interested
>>>in investigating how the lakes affect the local climate.
>>>
>>>How is lake ice treated? Unfortunately, the papers on Africa won't
>>>address that since
>>>they are for a warm climate.
>>>
>>>Does anyone know of papers using RegCM3 and the lake model for the
>>>Great Lakes?
>>>
>>>Thanks, Mike
>>>
>>>
>>>
>>>On Jun 28, 2007, at 8:33 AM, Richard Anyah wrote:
>>>
>>>
>>>
>>>>Hi Mike,
>>>>
>>>>The following publications may be relevant, though they use lake
>>>>model from variants of the RegCM family for Lake Victroia in
>>>>equatorial eastern Africa.
>>>>
>>>>
>>>>
>>>>
>>>>
>>>>
>>>>>I have some general questions about the lake model in RegCM3.
>>>>>In particular, relating to the Great Lakes.
>>>>>
>>>>>Could someone email me the references to some papers that use the
>>>>>lake model with regcm3? I would like to see previous applications
>>>>>
>>>>>
>>>>>
>>>>1. Song, Y., F.H.M. Semazzi and L. Xie, 2002: Development of a
>>>>coupled regional climate simulation model for the Lake Victoria
>>>>Basin. In /The East African Great Lakes,Limnology,Paleolimnology and
>>>>Biodiversity/, Odada E and Olago G(eds). Gordon and Breach:
>>>>Armsterdam: 141-154
>>>>
>>>>2. Song, Y., F.H.M. Semazzi and L. Xie, and L.J. Ogallo, 2004: A
>>>>coupled regional climate model for Lake Victoria basin of East
>>>>Africa. /Int. J. Climatol/. *24*, 57-75
>>>>
>>>>
>>>>3. Anyah, R.O., and F. H. M. Semazzi, 2004: Simulation of the
>>>>response of Lake Victoria basin climate to lake surface
>>>>temperatures./Theor. Appl. Climatol/,* 79, *55-69
>>>>
>>>>
>>>>4. Anyah, R.O., F.H.M. Semazzi and Lian Xie, 2006: Simulated
>>>>physical mechanisms associated with multi-scale climate variability
>>>>over Lake Victoria Basin in East Africa, Monthly Weather Review:
>>>>134,3588-3609
>>>>
>>>>
>>>>
>>>>>What dynamics does the lake model simulate? Lake ice fluctuations?
>>>>>Changes in lake level?
>>>>>
>>>>>
>>>>>
>>>> You may have to compute changes in E, P and horizonatal
>>>>mosture convergence to infer lake level fluctuations.
>>>> Also the 1D lake use simplified vertical exhange of moisture
>>>>and heat between the lake and the atmosphere.(See refs. 1, 2 and 4
>>>>above)
>>>>
>>>>
>>>>
>>>>>If the lake model is turned off, does the model assume
>>>>>climatological lake
>>>>>temperatures or is the lake replaced by land?
>>>>>
>>>>>
>>>>>
>>>>As far as I know when the lake is tuurned off, the "lake" surface
>>>>temperature uses the surface temperature, unless you physically
>>>>prescribe 'climatological' temperature over the lake surface
>>>>
>>>>
>>>>
>>>>Hope the information may be helpful.
>>>>
>>>>Richard
>>>>
>>>>--
>>>>------------------------------------------------
>>>>Richard Anyah
>>>>Research Associate
>>>>Center for Environmental Prediction
>>>>Department of Environmental Sciences
>>>>Rutgers University
>>>>14 College Farm RD
>>>>New Brunswick, NJ 08901-8551
>>>>Phone: (732) 932 9735
>>>>Fax: (732) 932 8644
>>>>-----------------------------------------------
>>>>
>>>>
>>>>
>>>>
>>>>
>>>>
>>>>
>>>>
>>
>>
--
------------------------------------------------
Dr. Richard Anyah
Research Associate
Center for Environmental Prediction
Department of Environmental Sciences
Rutgers University
14 College Farm RD
New Brunswick, NJ 08901-8551
Phone: (732) 932 9735
Fax: (732) 932 8644
http://www.envsci.rutgers.edu/~anyah
-----------------------------------------------
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