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H2OSOI goes beyond WATSAT #136
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Erik Kluzek < erik > - 2016-04-13 14:13:56 -0600 Hi Dominik Can you check which soil layer the max(h2osoi) ends up being? The top layer can exceed WATSAT because of ponding. And it looks like ponding is handled differently for urban versus other land-unit types. So you might check what the land-unit types are as well. Thanks for reporting the issue! |
** < Dominik.Rains > - 2016-04-15 03:58:30 -0600** Hi Erik, many thanks for the input. it is indeed the topmost layer, no urban areas in that specific area. As a side question: Can you suggest the best way of computing residual water content for each CLM pixel? Best regards, |
Erik Kluzek < erik > - 2016-04-18 12:01:55 -0600 Dominik I checked with Dr. Swenson our local hydrology expert. We don't calculate residual water content, anywhere so you'll have to figure it out based on it's definition. He also showed me that pond max is set to zero in clm45 for cesm1_2_1 (so likely cesm1_2_2 as well) for clm4_5 (although it's non zero for urban). So if you are getting WATSAT>H2OSOI for non-urban points in the first layer, that may indicate somethings wrong still. Can you tell us more about what version of the model you are using? |
** < Dominik.Rains > - 2016-04-19 05:50:07 -0600** Dear Erik, the version is cesm1_2_2 / clm4_5. Are there any basic checks we can perform to exclude a mistake on our side? A colleague also pointed me towards the paper 'http://journals.ametsoc.org/doi/abs/10.1175/2008JHM1011.1' but we are not sure if this is related. |
Looking at the latest code, there are certainly points where h2osoi is limited by watsat. But, I can't say that it's limited everywhere it should be. |
Hi all, |
The default calculation for the saturation water content or porosity (the CLM history field WATSAT) is described in the technical note here: See equation 2.7.49. |
** < Dominik.Rains > - 2016-04-12 07:47:23 -0600**
Bugzilla Id: 2306
Bugzilla CC: dlawren, rfisher, swensosc,
Bugzilla Attachment: watsat-max_sm.png - WATSAT - H2OSOI (areas masked where H2OSOI stays below saturation)
Created attachment 61
WATSAT - H2OSOI (areas masked where H2OSOI stays below saturation)
We are observing in our regional CLM 4.5 model setup, using a custom surface dataset and forcings, that over our simulation period H2OSOI often surpasses WATSAT significantly (~8%) in areas with high organic matter and precipitation.
We assume that, independently of our inputs, soil moisture should be constrained by WATSAT at all times.
The modeled catchment is the Murrumbidgee basin in Australia.
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