์ด๋ฒ ์ฃผ๋…
- TWS-NEE discussion with Sujan, Martin, Nuno, and Markus
- ๋ฐฅ & ์
2020. 11. 26. ๋ชฉ์์ผ
TWS-NEE discussion with Sujan, Martin, Nuno, and Markus
9์๋ถํฐ 11์๊น์ง ๋ด ์ฐ๊ตฌ๋ฅผ ์ด๋ป๊ฒ ์งํํด ์๊ณ ์ด๋ป๊ฒ ํด๋๊ฐ๋ฉด ์ข์์ง ํ ์ํ๋ ์๋ฆฌ๋ค.
๋ด ๋ฐํ๋ Sujan์ด ๋ง๋ค์ด์ค C-W coupled SINDBAD configuration์ ํ ์คํธํ๋ ๊ฒ ์์ฃผ๋ก ์งํ๋๋ค. Global run ์ํ ์ ์ site-level์์ ์ ๋ง๋์ง ํ์ธํด๋ณด๋ ๋จ๊ณ. ๊ทธ๋ฆฌ๊ณ ๋ช๋ช ๋ ผ๋ฌธ ์์ฝ.
Martin๊ณผ Markus๋ ์ฅ๊ธฐ ์ ๋ต์ ๋ํด ์กฐ์ธ์ ๋ง์ด ํด์คฌ๋ค. ๋ด ํ๋ก์ ํธ์ ์ฃผ์ ์ง๋ฌธ์ธ TWS-NEE IAV relationship์ ๋ฐ๋ก ํด๊ฒฐํ๊ธฐ ์ด๋ ต๋ค. ๋๋ฌธ์ ์๊ฒ ์ชผ๊ฐ์ ์ฌ์ด ๊ฒ ๋จผ์ ์งํํ๋ ๊ฒ์ด๋ค(divide&conquer). TWS IAV ํน์ NEE IAV๋ฅผ ๋จผ์ ์ดํด๋ด์ ๊ฐ๊ฐ component๊ฐ ๋ค๋ฅธ ๊ฒ์ ์ด๋ป๊ฒ ๋ฐ์ํ๋์ง, ์ด๋ค ๊ฒ ๊ฐ์ฅ ์ํฅ๋ ฅ ์๋์ง ๋ฑ์ ๋จผ์ ์ดํผ๋ฉด ์ข ๋ ๋ด ์ง๋ฌธ์ ๋ช ํํ๊ฒ ๋๋ ์ ์์ ๊ฒ ๊ฐ๋ค. ๋ฏธํ ํ Martin์ด ์ฝ๋ฉํธ๋ฅผ ์ ๋ฆฌํด์ ๋ฉ์ผ๋ก ๋ณด๋ด์คฌ๋ค.
Hi Hoonteak,
thanks again for the talk and all for the discussion. I briefly write again my main comments, for clarity, and transparency.
It’s really great and important that you started diving into SINDBAD! For this stage of the PhD and esp for the PAC it’s important to get also the problem and concept clear, and a tentative plan of attack straight. Markus suggestion on how different TWS components may be interacting with different C cycle processes on scales relevant to this project would also help to get things clearer conceptually.
With divide and conquer I was referring to trying to identify relevant chunks of lower complexity which could form papers or work packages, rather than starting with full complexity. In my opinion you can divide the problem in two bigger pieces: a) getting TWS IAV ‘right’, b) getting NEE IAV (and trend) right. Of course we expect some interactions, so we need to put them together, but maybe not from the beginning.Starting from TWS IAV would be conceptually nicer as the water cycle constraints are likely more important for the carbon cycle IAV than carbon cycle constraints on water cycle IAV. But getting TWS IAV right might also be a ‘trap’ for a first project. To understand this better it would be good to analyse Tina’s and Basil’s results with respect to TWS IAV. In particular we’d like to infer which processes and data constraints might be missing or how difficult it may be (or not). My gut feeling is that we have a problem with surface water storage variations. To look at this you can look at regions and times where this should matter most, compared to other regions. For example surface water storage variations should matter most in the wet period of the wet tropics (esp amazon), and during/after snow melt in the high-latitude snow regions … or other regions with high inland water body area. As far as I remember the global TWS IAV is controlled by the tropics where e.g. Tina’s model doesn’t get it while it wasn’t too bad in other regions. But maybe you find other things!
Starting with global NEE IAV and trend is in my opinion also a viable strategy. Keenan (https://www.nature.com/articles/ncomms13428) showed that you can capture the big picture decadal variability / trend with a simple light use efficiency model with CO2 fertilization and Mirco’s no-pool TER model. Constraining CO2 fertilization with a global long-term inversion should really not be difficult, even when starting with a very simple (and fast) respiration model. Getting the NEE IAV on ‘eye-level’ with TRENDY models should also not be difficult - also FLUXCOM get’s the patterns (not the variance correct though) without having any carbon pool. I’m certainly not arguing that we shouldn’t have C pools in the model but i would start with something simple. Land use change aspects had basically no relevant effect on global NEE IAV in trendy models. Let’s assume that with a relatively simple setup we can get global NEE IAV and trend reasonable one could look at the effect of co2 fertilization on (spatial) NEE IAV variance changes with factorial experiments (to have an interesting research question :)).
When trying to make some progress on global NEE IAV beyond state-of-the art (which is maybe not necessary but would be nice) you’ll encounter probably three things: a) the vulcano eruptions, b) the change in variance, and c) something going on in the wet tropics. Wrt a) most people think it’s related to diffuse radiation which is not or not well represented in global meteo forcing data and/or models. I know that Stephen Sitch and Lina Mercado were after generating a better radiation product for that. We can ask … ; for b) it’s still unclear as far as i know; for c) it could be a ‘wet’ stress signal (either suppression of respiration, or wet stress on GPP … GPP of tropical forests seem quite sensitive to VPD otherwise.Starting with the NEE would have also some advantage in terms of learning from Tina - in her final analysis over the next months she’ll look at the effect of lateral fluxes/river routing on TWS variations… so there are pros and cons for starting with TWS or NEE. I would try to start with whatever seems easier and more straightforward to you. But it does matter of course for your sindbad setup as you need different model structures, data constraints, and forcing data (e.g. long-term for nee).
Wrt attribution problem and the different methods you read about: Most of them were ‘empirical’ and for using with ‘observations’ only. If we have a model explaining the observations we should focus on using the model to do attribution, e.g. by designing factorial experiments, and by understanding equifinality due to parameter uncertainties.
Sorry for the long email. Trying to compensate a bit for my lack of availability over the next weeks:) Looking very much forward to this journey and more in-depth discussion!
cheers,
martinP.S.: Sooner or later you’ll likely encounter different opinions and suggested directions. Sujan is your main adviser here and Matthias in Dresden so discuss and decide together with them in case of conflicts. It’s important to prioritize to make progress, not always you can make everyone happy simultaneously.
๋ฏธํ ํ Sujan๊ณผ ์ถ๊ฐ ๋ฏธํ ์ ํ๊ณ , TWS IAV ๋จผ์ ์์ํด๋ณด๊ธฐ๋ก ํ๋ค. Tina์ Basil์ด ํ ๊ฒ์ ํ ๋๋ก. ๊ทธ๋ฆฌ๊ณ Cluster ์์ ์ ๋ ์ต์ํด์ง๊ธฐ ์ํด Linux๋ฅผ ์ฌ์ฉํด๋ณด๊ธฐ๋ก ํ๋ค.
2020. 11. 28. ํ ์์ผ
์ค๊ตญ ์ ๋ค๊ณผ ์ ๋ & ํ ์ ํ๋ค. ์ด๋ฒ์ ๋ด๊ฐ ์ข ๋ง๋ค์ด ์คฌ๋ค. ๋ฉ๋ด๋ (์ต๊ทผ์ ๋ฐฐ์ด) ๋ก๋ณถ์ด, (๊ทธ๋ ์์นจ ์๋ง๊ฐ ๋ ์ํผ๋ฅผ ๋ณด๋ด์ค) ์์ธ์ง ์ผ์ฑ ๋ณถ์, ๊น์น์ฐ๊ฐ๋ค. ์ด๋ฅผ ์ํด ํ๋คํ๋ค์์ (๋๋์ด) ๊น์น๋ฅผ ์ฌ์๋ค. ์… ๋์ฒด๋ก ๋ง์กฑ์ด๋ค. ๋ก๋ณถ์ด๋ ์ด๋ฌต ๋ง์ด ์ข ์๋ฌ์์ง๋ง ๋ค์๋ถํฐ ๋ถ์ฐ์ด๋ฌต ์ฌ ์ฐ๋ฉด ๋ ๊ฒ ๊ฐ๋ค. ๊ณ ์ถง๊ฐ๋ฃจ๋ฅผ 1T๋ง ์ด ๊ฒ๋ ์ ๋จนํ๋ค. ์์ผ๋ณถ์ ์์ธ์ง๊ฐ ์๋ฌ. ๋ ์ผ ์์ธ์ง๋ ๋์ฒด๋ก ์ง๋ค. ๊น์น์ฐ๊ฐ๋ ๊น์น๊ฐ ๋๋ฌด ์ค์ต์ด์ ์๋ฌ์์ง๋ง ๊ทธ๋๋ ๋จน์๋งํ๋ค.
์ ์ ๋ฐ๋ปํ ๋ ๋์์ธ –> ๋ณด๋์นด+๋ ๋ชจ๋ค์ด๋ –> ๊ณ ๋์ฃผ. ์ ์ผํ๊ฒ ์ ์ํ๊ณ ์ข์ํ๋ ์ค๊ตญ ์น๊ตฌ๊ฐ ๊ณ ๋์ฃผ๋ฅผ ๊ฐ์ง๊ณ ์์๋ค. ๋ด๊ฐ ์ข ๋ง์๋ ๋ฏ ํด๋ณด์ธ๋ค๋ฉด์ ์คํผ์ค์์(?!) ๊ณ ๋์ฃผ๋ฅผ ๊ฐ์ ธ์์คฌ๋ค. ๋ณด๋์นด๋ณด๋ค๋ ๋ง์์๋๋ฐ ์ข ์๋ค (52%).
2020. 11. 29. ์ผ์์ผ
๊น์น์ ํจ๊ป ์ฐ ๋์ฅ, ๋๋ถ. ๋๋์ด ๋์ฅ์ฐ๊ฐ๋ฅผ ํด๋จน๋๋ค. ์ญ์ ๋์ฅ์ฐ๊ฐ๋ ๋ฐฅ์๋ค ์ฅ์ญ์ด๋ค.
๊ทธ ์ธ…
- ์ฌ ๊ฐ์ ์ฒ์์ผ๋ก ์๋ฆฌ๊ฐ ๋ด๋ ธ๋ค. ๋ ๋ด๋ฆฐ ํ๊ฒฝ์ด ๊ธฐ๋๋๋ค. ์ด์ฌ ๊ฐ๊ธฐ ์ ์ ๋์ด ์ฌ๊น.
- ์์ฑ๋ ์๋ ์ ์์ ์ฑ๊ณต์ ์ด์๋ ํ์คํ
- ํฌ๋ฆฌ์ค๋ง์ค ๋จ์ฅํ ๊ดดํ ๊ฐค๋ฌ๋ฆฌ. ๋ธ๋ญ๋ง๋ค ๋ํ๋ฅผ ๋ฌ์ฌํ ์ธํ๋ค์ด ์์๋ค. ๋ฐฑ์ค๊ณต์ฃผ, ๋นจ๊ฐ ๋งํ …. ์ ๋๋๋ ์ฌ์ง์ด ๋ค์จ/๋ ์จ์ ๋ง์ถฐ ์์ง์ด๊ธฐ๊น์ง ํ๋ค. ๋ ์ผ์ ๋ฌ๊ธ ์๋ ๊ณณ์์ ๋ํ ์ผํ๋ค.
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