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Support of inclusion of **_FVCOM_** into **_UFS-Coastal_**. Three tasks are defined for this project:
- **_Development:_** Contributions to the **_FVCOM_** repository in the model's source code and iโฆ
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The em apps are great and I will start using them in my class this week!
The only app that I cannot find and would be useful is to calculate resistivity sounding curves for 1D layered models (using eโฆ
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๐งฌโก๏ธ๐ง โก๏ธ๐ปโก๏ธ๐
{ฮฃ = ๐(๐ญ๐)}
while ๐:
๐งฌ.append(๐งฌ[-1].evolve())
if ๐งฌ[-1].complexity > ฮ:
๐ง = ๐งฌ[-1].emerge()
๐ป = ๐ง .create()
๐ = ๐ป.simulate()
if ๐.contains(๐งฌ):
โฆ
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Fabrice,
I have two questions about ngspice appearance in the PySpice documentation:
Chapt. 5.1
The main drawback of Ngspice is to inherit the old C code base of Berkeley SPICE.
Why do you conโฆ
holvo updated
3 years ago
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Batch computation is a feature that's been requested a few times. The idea is that you want to run many simulations of identical systems, or perhaps just evaluate the energies of many conformations. โฆ
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Hello. I am currently using Mac M1. And running the following code ( the file in ```/spyro/paper/run_fwi_2d.py```). It shows the error from the pybind11 ``` ROL.Algorithm("Line Search", params)```. Dโฆ
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[์ ์ฒด ์๋ฎฌ๋ ์ด์
]
1. ๋๋น์ ์คํก์ค ๋ฐฉ์ ์ ๊ทผ์ฌํ๋ ๊ณผ์ ์ค๋ช
ํ๊ธฐ
2. ์ ์ฒด ์๋ฎฌ๋ ์ด์
์ ์ฒด ์๋ ฅ์ด ํํ๋์ง ์๋ ์ด์ (์๋ง๋ ํ๋ฉด๋ง ๊ณต์์ ์งฐ๊ธฐ ๋๋ฌธ)
-> ๋๋น์ ์คํก์ค ๋ฐฉ์ ์์ ํ๋์ง, shallow water eq๋ฅผ ์ฌ๋ฌ๋ฒ ๊ฒน์ณ์ ํ๋์ง
3. ์๋ฎฌ๋ ์ด์
ํ๋ ๋ฐฉ๋ฒ ๋ฐํ ์์๋ฅผ ๋ฐ๊พธ๋๊ฐ ์ ์ธํ๊ธฐ
[๋ฐํ ์ ๊น์ง ํ ๊ฒ]
1. โฆ
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**Intro**
I was trying to measure the performance impact of a single cache miss while reading the middle element of an array containing 1,000,000 integers. It required 0.437 ns according to benchmaโฆ
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I'd like to open a discussion thread to get the status of developments with regard to the use of Machine Learning techniques in Argo QC procedures.
Different groups may have started to explore thiโฆ
gmaze updated
4 years ago
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I think the simulation of ClassicDSD has rounding / precision issues.
When does the issue arise?
When simulation CRN in ClassicDSD where the rate constants are numbers with very different magnitudโฆ