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Temporal and spatial scales of lake processes. Part 1: physical and ecological scales, non-dimensional parameters and flow regimesView Crossref metadata(active tab) <div id="edit-xml" class="form-item form-type-item"> <?xml version="1.0"?> <doi_batch version="4.4.1" xmlns="http://www.crossref.org/schema/4.4.1" xmlns:jats="http://www.ncbi.nlm.nih.gov/JATS1" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.crossref.org/schema/4.4.1 http://www.crossref.org/schemas/crossref4.4.1.xsd"><head><doi_batch_id>000690</doi_batch_id><timestamp>1713595718</timestamp><depositor><depositor_name>University of the Aegean</depositor_name><email_address>uoa@university.com</email_address></depositor><registrant>Global NEST Journal</registrant></head><body><journal><journal_metadata><full_title>Global NEST Journal</full_title><full_title>Global NEST: the international Journal</full_title><issn media_type="print">1790-7632</issn><issn media_type="electronic">2241-777X</issn></journal_metadata><journal_issue><titles><title>Issue 4</title></titles><publication_date><month>12</month><year>2024</year></publication_date><journal_volume><volume>13</volume></journal_volume><issue>4</issue></journal_issue><journal_article><titles><title>Temporal and spatial scales of lake processes. Part 1: physical and ecological scales, non-dimensional parameters and flow regimes</title></titles><abstract xmlns="http://www.ncbi.nlm.nih.gov/JATS1"><p>Scaling concepts, related to basic physical transport and mixing processes and other ecological aspects in lakes, are reviewed in an ecohydrodynamic perspective; the length and time scales as well as the non-dimensional parameters governing the various flow regimes and relevant to these processes are also presented, emphasizing the influence they have on lake ecosystems. The hierarchy of length scales is very important in determining both the turbulence structure, and in affecting the ecological processes occurring in lakes. Most of these scales are defined in terms of several basic parameters which, when combined properly, yield important dimensionless numbers, as: Rf, Ri, Pr, T, Ret, Frt, Grt, and Prt, the flux and gradient Richardson numbers, the Prandtl number, a dimensionless time, and the turbulent Reynolds, Froude, Grasshof and Prandtl numbers, respectively. A few more dimensionless numbers (as the Lake and Wedderburn numbers, LΝ, W, etc.) are also useful in characterizing the general dynamic behavior of lakes. Ratios of length or time scales may also provide similar useful parameters. </p></abstract><publication_date><month>04</month><day>30</day><year>2013</year></publication_date><pages><first_page>339</first_page><last_page>353</last_page></pages><publisher_item><identifier id_type="pii">737</identifier></publisher_item><doi_data><doi>10.30955/gnj.000737</doi><timestamp>1713595718</timestamp><resource>https://journal.gnest.org/publication/737</resource></doi_data></journal_article></journal></body></doi_batch> </div>
