method of calculating the maximum water flow in the mountains

Clicks: 123
ID: 225733
2015
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
Steady

Ranked #33 of 39 articles by views in progress in nuclear energy

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
The Befani-Gopchenko model is suggested to calculate the maximum water expense in the absence of hydrological observations. The model is a combination of reduction, dimensional and critical intensity methods used in normative practice in the majority of world countries. Statistical analysis of time-series observations is applied, and the methods to define parameters and coefficients in the model are suggested. Their spatial distribution corresponds to general geographical properties of hydrographic characteristics in the mountains and is offered to calculate the maximum flood runoff. The applied method contains useful information to help prepare regional normative acts to define major constructive components of hydrological estimations of maximum water runoff.
Reference Key
v.2015aerulmethod Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors ;YAVKIN V.;GOPCHENKO E.
Journal progress in nuclear energy
Year 2015
DOI
10.17378/AWC2015_26
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.