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Description
The simulation that Jessie analysed to make this plot
has a large source in the mid 20th C, which is outside the range of TRENDY. I want to understand how it differs from TRENDY, what evidence we have IRL that TRENDY is accurate for this time period, and whether that evienc contradicts FATES outputs.
Charlie's simulations show that rangeland clearing is driving much of the source.
The GCB NBP 'constraint' has most models being almost neutral at the beginning, with CanESM gaining ±10PG before all becoming sources:

But the GCB plots have the LUC fluxes (from bookeeping?) being notably higher than the 'land sink', suggesting that their assessment is that the land is actually a source pre-1980-90ish.
The data from the GCB website, downloaded into this file
https://docs.google.com/spreadsheets/d/1csQx6wnh1gClzSAwpo1wnYuYDAPI_h-ZGvXPy8xhvfE/edit?gid=0#gid=0
look like this
Which seems to inducate that the yellow-light green inthe above plot collectively become a net sink shortly after 1960.
From this paper we get the breakdown of TRENDY into components, and the 'benchmark' which starts in 1960 is after the part where it assessed the land to be a slight source.
https://agupubs.onlinelibrary.wiley.com/doi/pdfdirect/10.1029/2024GB008102
we get this plot

For the NH we have
FATES
Randerson et al
I have not got my thoughts fully together on this, but at least these are some basic plots to compare with...