PNNL-TES / GlobalC

A topdown and bottom up approach for global C cycle
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Consequences #3

Open bpbond opened 5 years ago

bpbond commented 5 years ago

What if GPP is really 150 PgC/yr, not 125?

What is Rs is really 60 Pg C/yr, not 85?

bpbond commented 5 years ago

Also "The results suggest that previous eddy-covariance-based estimates of global photosynthesis and respiration are probably biased high" Keenan et al. 2019

bpbond commented 5 years ago

From Nature brief: "The data could mean that the world's landmasses are taking up 7% more C than scientists thought" re https://www.atmos-chem-phys.net/19/8687/2019/

bpbond commented 5 years ago

"Model uncertainty—as measured by intermodel spread—is high for soil carbon turnover time (τ) and exceeds the uncertainty estimated for carbon uptake through gross primary production (GPP) (15, 16)." https://science.sciencemag.org/content/353/6306/1419

jinshijian commented 5 years ago

2019-9-4 meeting summary (1) Cut GPP and RS estimates after 1985 or 1990. (2) Comparing with CMIP6 GPP. (3) Think about implications: a. ESMs may be calibrated against wrong benchmark numbers; b. terrestrial C turnover time may be wrong; c. how can this change our understanding of global carbon cycling?

2019-9-9 meeting summary (1) Give GPP more categories (2) Try to break GPP down to high, middle, and tropic

bpbond commented 5 years ago

Why might Rs be too high? Perhaps soil moisture effects we're not accounting for? E.g. cite Stocker et al. (2019).