A Comparison of Several “Single-Pass” Estimators of the Standard Deviation of Wind Direction

Clicks: 144
ID: 268058
1984
Article Quality & Performance Metrics
Overall Quality
Not rated
Combines reader engagement with the AI quality analysis. This article has not been analysed, so there is no overall score — reader engagement is measured and shown alongside.
AI Quality Assessment
Not analyzed
Readership in this journal
Popular

Ranked #5 of 7 articles by views in journal of applied meteorology and climatology

Most read Least read

Bar heights use a square-root scale.

Mint this article as an NFT
Not yet minted

Create a permanent, verifiable on-chain record of this article on the Scimatic Network. The NFT is held in your Journament account, and you can withdraw it to your own wallet at any time.

5 SUSD one-off · no wallet required
Abstract
AbstractComputation of the standard deviation of wind direction σθ generally requires repeated consideration of the individual measurements of wind direction. This need for multiple passes through the data sample can create a storage problem for small or remote data acquisition systems. Statistical quantities that can be computed during a single pass through incoming wind speed and direction data are first reviewed, and relationships between these quantities are discussed. A single-pass estimator for σθ is then developed and found to correspond to within ±2% of conventional, two-pass σθ computations for unimodal angular distributions spanning the full σθ range of from 0 to 103.9°. Similar comparisons are presented for other, recently proposed estimators of σθ.
Reference Key
yamartino1984journala Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors R. J. Yamartino;
Journal journal of applied meteorology and climatology
Year 1984
DOI
10.1175/1520-0450(1984)0232.0.CO;2
URL
Keywords

Citations

No citations found. To add a citation, contact the admin at info@scimatic.org

No comments yet. Be the first to comment on this article.