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Record W7030463508

Numerical Approaches for Time Integration of Atmospheric Models

2024· other· en· W7030463508 on OpenAlexaboutno aff

Bibliographic record

VenueeScholarship (California Digital Library) · 2024
Typeother
Languageen
FieldMathematics
TopicNumerical methods for differential equations
Canadian institutionsnot available
Fundersnot available
KeywordsNumerical weather predictionIntegratorEulerian pathTime delay and integrationAtmospheric modelNumerical integrationEuler equationsEuler's formulaAtmosphere (unit)Stiff equation
DOInot available

Abstract

fetched live from OpenAlex

Numerical weather prediction (NWP) involves solving equations that govern the evolution of the atmosphere over the time intervals of interest, in other words an initial value problem for evolution equations is solved with the current state of the atmosphere treated as the initial condition. The computational time and spatial scale of NWP models involve large scale atmospheric dynamics such as planetary waves, tropical cyclones, gravity waves, acoustic waves, and more. One of the major computational difficulties in NWP is the wide varying propagation speeds of the atmospheric waves. The resulting stiffness from the fast-slow waves encourages the development of more efficient time integrators for efficient and accurate weather forecasting.The majority of weather centers use a semi-implicit semi-Lagrangian (SISL) time integrator. The semi-Lagrangian method is unconditionally stable for the transport equation, and therefore allows for stable integration of the atmospheric model with time steps larger than Eulerian methods. However, SISL methods develop resonance in the presence of mountains. Many tried to address this issue with additional damping, diffusion terms, or adjusting the coefficient of the time integrator, but the techniques can lead to order reduction in the time integration and can affect the overall accuracy of the solution. The presence of resonance has re-incentivized research directions back to an Eulerian formulation of the atmospheric models. In this dissertation, we explore two directions of research for improving the time integration of NWP models. First, exponential integrators have demonstrated to be a computationally efficient and accurate method for the shallow water equations and the Euler equations. Therefore, exponential integrators are a viable choice for NWP. We improve upon the parallel performance of exponential integrators on high performance computing platforms for large-scale, massively parallel environments, consequently making them a more practical choice for NWP. Second, it will take time to transition to a new operational model. Many forms of validation with other models such as ocean, air quality, climate, and more, must be cleared in order to fully adopt a new proposed scheme. Therefore, it is still beneficial to continue to improve upon the current SISL methods. Thus, we address the problem of resonance by replacing the Crank-Nicolson time integrator in the Canadian Global Environmental Multiscale model with a second order backward difference formula time integrator.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.002
metaresearch head score (Gemma)0.007
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Simulation or modeling · Consensus signal: none
GenreCandidate signal: Methods · Consensus signal: Methods
Teacher disagreement score0.007
Threshold uncertainty score0.025

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0020.007
Meta-epidemiology (narrow)0.0010.001
Meta-epidemiology (broad)0.0010.002
Bibliometrics0.0010.001
Science and technology studies0.0010.002
Scholarly communication0.0030.002
Open science0.0030.003
Research integrity0.0020.004
Insufficient payload (model declined to judge)0.0070.002

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.077
GPT teacher head0.290
Teacher spread0.213 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designSimulation or modeling
Domainnot available
GenreMethods

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations0
Published2024
Admission routes1
Has abstractyes

Explore more

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