{"refrec":{"BRefID":12998,"RR":"<b>van der Veer, H.W.</b> (1983). Een model voor de schatting van de watermassa met hoogwater op de platen van het Balgzand. <i>Interne verslagen Nederlands Instituut voor Onderzoek der Zee</i>, 1983(9). NIOZ: Texel. 12 pp.","BEntID":12998,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". <i>Interne verslagen Nederlands Instituut voor Onderzoek der Zee</i>, 1983(9). NIOZ: Texel.  12 pp.","DocTypID":13,"DocType":"Reports","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"van der Veer, H.W.","OrigTitleTranslFlag":1,"Authorstringtrunc":"van der Veer, H.W.","Englishabstract":"This report describes the influence of wind stress on the water level with high water on the Balgzand, a tidal shelf area in the western Wadden Sea. Up to BF 2 no influence of windstress is detectable. From BF 3 on wind blowing from the sector ENE to SSW results in a decreased water-level, while for the remaining sector an increased level is observed. With the aid of the real observed high water-level of the nearby situated station \"Den Helder\" and the prevailing wind regime, an accurate prediction of expected water-levels on different locations on the Balgzand is possible. With some characteristics of the Balgzand area an estimate of the total watermass covering the area with high water can be made.","AbstractOtherLang":"In dit onderzoek wordt aan de hand van peilschaal registraties de invloed van het windregiem op de waterstand met hoogwater op de platen van het Balgzand beschreven. Windsterkten tot BF 2 hebben geen invloed op de waterstand. Een hogere windsterkte komende uit de sector ONO tot wzw zorgt voor een verlaagde waterstand, terwijl wind uit de resterende sectoren een verhoging betekent. Het blijkt mogelijk om uitgaande van de werkelijke hoogwaterstand van het nabijgelegen \"Den Helder\" met behulp van het windregiem een nauwkeurige schatting te geven van de te verwachten waterstanden op het Balgzand. Hieruit kan vrij eenvoudig een goede schatting van de watermassa op het gebied met hoogwater gemaakt worden.","BibLvlCode":"MS","StandardTitle":"Een model voor de schatting van de watermassa met hoogwater op de platen van het Balgzand","OrigTitleLangCode":"nl","OrigTitleLangCodeExtended":"dut","OrigTitleLangID":41,"DateLastModified":{"date":"2025-07-22 01:33:06.175990","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":null,"MonPub":1983,"DateUpdate":"2025-07-15","DateCreate":"2001-07-06","SecASFANote":null,"ConfID":null,"PeerRev":0,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1},"refs":null,"anarec":null,"monrec":{"MonID":12998,"ISBN":null,"PubliDate":1983,"IssueDate":null,"Volume":"1983","Issue":"9","Pagination":"12","Place":"Texel","Edition":null,"BRefXtra":null,"BRefXtraRR":null,"SerID":5036,"SerRR":"Interne verslagen Nederlands Instituut voor Onderzoek der Zee. 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