... | @@ -118,10 +118,10 @@ first runs did not work because of something in the newly made river input files |
... | @@ -118,10 +118,10 @@ first runs did not work because of something in the newly made river input files |
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<img src="uploads/0583ccd90f5e2fb294626a0adc958ddc/image.png" width=49%>
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<img src="uploads/0583ccd90f5e2fb294626a0adc958ddc/image.png" width=49%>
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<img src="uploads/b4ace1fc3265be5248ea5b1050d2aec2/image.png" width=49%>
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<img src="uploads/b4ace1fc3265be5248ea5b1050d2aec2/image.png" width=49%>
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The difference decrease in `LS400`, but the interesting bit here, is that we loose DIC compare to the `no-river` run, although we add the river nutrients...
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The difference decrease in `LS400`, but the interesting bit here, is that we loose DIC compare to the `no-river` run, although we add the river nutrients...
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Looking at the river, we might understand what's going on :
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Looking at the river, we might understand what's going on :
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Here `LS200`:
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Here `LS200`:
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<img src="uploads/21b7054deefbdae89b3eaf6395662829/image.png" width=49%>
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<img src="uploads/21b7054deefbdae89b3eaf6395662829/image.png" width=49%>
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<img src="uploads/d627423cc33edc7804850527fdaa68de/image.png" width=49%>
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<img src="uploads/d627423cc33edc7804850527fdaa68de/image.png" width=49%>
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The problem seems to come from the mismatch between DIN and DIC riverine inputs. PP is boosted by the N supply, where no DIC is added and where fresh water arrives. DIC is driven down by the PP, and probably bellow 0.0 because of the fresh water and advection.
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The problem seems to come from the mismatch between DIN and DIC riverine inputs. PP is boosted by the N supply, where no DIC is added and where fresh water arrives. DIC is driven down by the PP, and probably bellow 0.0 because of the fresh water and advection.
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