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  <doi_batch_id>aspg-24-4492-1791482590</doi_batch_id>
  <timestamp>20261008180310</timestamp>
  <depositor>
   <depositor_name>American Scientific Publishing Group</depositor_name>
   <email_address>admin@americaspg.com</email_address>
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  <registrant>American Scientific Publishing Group</registrant>
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  <journal>
   <journal_metadata language="en">
    <full_title>Journal of Neutrosophic and Fuzzy Systems</full_title>
    <abbrev_title>JNFS</abbrev_title>
    <issn media_type="print">2771-6430</issn>
    <issn media_type="electronic">2771-6449</issn>
   </journal_metadata>
   <journal_issue>
    <publication_date media_type="online">
     <year>2026</year>
    </publication_date>
    <journal_volume>
     <volume>11</volume>
    </journal_volume>
    <issue>2</issue>
   </journal_issue>
   <journal_article publication_type="full_text">
    <titles>
     <title>Persistent Choquet Fuzzy Evidence for Detecting and Attributing Distribution Drift in Data Streams</title>
    </titles>
    <contributors>
     <person_name sequence="first" contributor_role="author">
      <given_name>Rama Asad</given_name>
      <surname>Nadweh</surname>
      <affiliations>
       <institution>
        <institution_name>Department of Science and Information Technology, Islamic Online University, Doha, Qatar</institution_name>
       </institution>
      </affiliations>
     </person_name>
    </contributors>
    <jats:abstract>
     <jats:p>Data-stream drift is rarely one-dimensional: a changed stream may move in location, inflate in scale, alter its tail geometry, or differ globally even when no single moment changes decisively. This paper develops a fuzzy monitoring layer for a scalar stream zt ∈ R by comparing adjacent windows At and Bt through four robust evidences dj,t : median displacement, robust log-scale change, interquantile tail-shape change, and normalized one-dimensional transport. Stationary calibration maps each dj,t to a fuzzy grade uj,t ∈ [0,1]. A normalized 2-additive capacity then aggregates the evidence by qt = 4Σ j=1 mjuj,t +Σ j&lt;k mjk min(uj,t ,uk,t ) ∈ [0,1], so pairwise reinforcement is modeled explicitly rather than hidden inside an arithmetic score. Persistence is separated from instantaneous evidence through At = [λAt−1 +qt −δ]+, and an alarm occurs when At ≥ h. The resulting Persistent Choquet Fuzzy Drift Monitor (PCFDM) also admits an exact component decomposition qt = Σj φj,t for drift attribution. A reproducible Monte Carlo study uses 120 independent stationary calibration streams and 220 test replications for each of seven scenarios. At matched stream-wise calibration, PCFDM detects mean, scale, mixed, and gradual drifts in 94.5%, 89.5%, 95.0%, and 92.3% of runs, with median delays 72, 88, 72, and 192 samples. Its transient-shock alarm rate is 40.5%, compared with 49.1% for fuzzy-mean evidence, 76.8% for maximum fuzzy evidence, and 65.9% for transport alone. Heavy-tail drift remains more difficult (48.2% detection), revealing a genuine trade-off between persistent multi-evidence confirmation and sensitivity to isolated shape changes. The contribution is therefore a mathematically decomposable fuzzy evidence mechanism for monitoring and explaining drift, not a claim of universal dominance over specialized change detectors.</jats:p>
    </jats:abstract>
    <publication_date media_type="online">
     <year>2026</year>
    </publication_date>
    <pages>
     <first_page>09</first_page>
     <last_page>16</last_page>
    </pages>
    <publisher_item>
     <item_number item_number_type="article-number">4492</item_number>
    </publisher_item>
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     <ai:license_ref applies_to="vor">https://creativecommons.org/licenses/by/4.0/</ai:license_ref>
    </ai:program>
    <doi_data>
     <doi>10.54216/JNFS.110202</doi>
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