{"refrec":{"BRefID":355172,"RR":"<b>van Haren, H.; Bosveld, F.C.</b> (2022). Internal wave and turbulence observations with very high-resolution temperature sensors along the Cabauw Mast. <i>J. Atmos. Oceanic. Technol. 39(8)</i>: 1149-1165. <a href=\"https://dx.doi.org/10.1175/jtech-d-21-0153.1\" target=\"_blank\">https://dx.doi.org/10.1175/jtech-d-21-0153.1</a>","BEntID":352885,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>J. Atmos. Oceanic. Technol. 39(8)</i>: 1149-1165. <a href=\"https://dx.doi.org/10.1175/jtech-d-21-0153.1\" target=\"_blank\">https://dx.doi.org/10.1175/jtech-d-21-0153.1</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"van Haren, H.; Bosveld, F.C.","OrigTitleTranslFlag":0,"Authorstringtrunc":"van Haren, H.; Bosveld, F.C.","Englishabstract":"<p>    Knowledge about the characteristics of the atmospheric boundary layer is    vital for the understanding of redistribution of air and suspended contents    that are particularly driven by turbulent motions. Despite many modeling    studies, detailed observations are still demanded of the development of    turbulent exchange under stable and unstable conditions. In this paper, we    present an attempt to observationally describe atmospheric internal waves    and their associated turbulent eddies in detail, under varying stableconditions. Therefore, we mounted 198 high-resolution temperature (    <em>T</em>) sensors with 1-m spacing on a 200-m-long cable. The    instrumented cable was attached along the 213-m-tall meteorological mast of    Cabauw, Netherlands, during late summer 2017. The mast has standard    meteorological equipment at extendable booms at six levels in height. A    sonic anemometer is at 60 m above ground. The <em>T</em> sensors have a    time constant in air of <em>τ<sub>a</sub></em> ≈ 3 s and an apparent drift    about 0.1°C month<sup>−1</sup>. Also due to radiation effects, short-term    measurement instability is 0.05°C h<sup>−1</sup> during nighttime and 0.5°C    h<sup>−1</sup> during daytime. These <em>T</em>-sensor characteristics    hamper quantitative atmospheric turbulence research, due to a relatively    narrow inertial subrange of maximum one order of magnitude. Nevertheless,    height–time images from two contrasting nights show internal waves up to    the buoyancy period of about 300 s, and shear and convective deformation of    the stratification over the entire 197-m range of observations, supported    by nocturnal marginally stable stratification. Moderate winds lead to    20-m-tall convection across weaker stratification, weak winds to episodic    <10-m-tall shear instability across larger stratification.</p>","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Internal wave and turbulence observations with very high-resolution temperature sensors along the Cabauw Mast","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-10 01:32:45.604441","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Boundary-layer meteorology; High-resolution temperature sensors; Internal waves; Mast observations; Stratified turbulence","OtherDescriptors":null,"Notes":null,"AnaPub":2022,"MonPub":null,"DateUpdate":"2022-08-29","DateCreate":"2022-08-29","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000848563300005","VABBcode":null,"OpenAcc":1,"DOI":"10.1175/jtech-d-21-0153.1"},"refs":null,"anarec":{"AnaID":355172,"PubliDate":2022,"Pagination":"1149-1165","XtraPublOfAnaID":null,"ISBN":null,"Volume":"39","Issue":"8","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":45630,"SerRR":"Journal of Atmospheric and Oceanic Technology. American Meteorological Society: Boston, MA.  ISSN 0739-0572; e-ISSN 1520-0426","StandardTitleSer":"Journal of Atmospheric and Oceanic Technology","ISSN":"0739-0572","AbbrevSer":"J. Atmos. Oceanic. 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