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{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2023,12,20]],"date-time":"2023-12-20T00:36:22Z","timestamp":1703032582819},"reference-count":59,"publisher":"Copernicus GmbH","issue":"24","license":[{"start":{"date-parts":[[2023,12,19]],"date-time":"2023-12-19T00:00:00Z","timestamp":1702944000000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"DOI":"10.13039\/501100001659","name":"Deutsche Forschungsgemeinschaft","doi-asserted-by":"publisher","award":["project number 268020496 \u2013 TRR 172"]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Atmos. Chem. Phys."],"abstract":"<jats:p>Abstract. This study evaluates methods to derive the surface mixing layer (SML) height of the Arctic atmospheric boundary layer (ABL) using in situ measurements inside the Arctic ABL during winter and the transition period to spring. An instrumental payload carried by a tethered balloon was used for the measurements between December 2019 and May 2020 during the year-long Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition. Vertically highly resolved (centimeter scale) in situ profile measurements of mean and turbulent parameters were obtained, reaching from the sea ice to several hundred meters above ground. Two typical conditions of the Arctic ABL over sea ice were identified: cloudless situations with a shallow surface-based inversion and cloudy conditions with an elevated inversion. Both conditions are associated with significantly different SML heights whose determination as accurately as possible is of great importance for many applications. We used the measured turbulence profile data to define a reference of the SML height. With this reference, a more precise critical bulk Richardson number of 0.12 was derived, which allows an extension of the SML height determination to regular radiosoundings. Furthermore, we have tested the applicability of the Monin\u2013Obukhov similarity theory to derive SML heights based on measured turbulent surface fluxes. The application of the different approaches and their advantages and disadvantages are discussed.\n <\/jats:p>","DOI":"10.5194\/acp-23-15473-2023","type":"journal-article","created":{"date-parts":[[2023,12,19]],"date-time":"2023-12-19T07:04:41Z","timestamp":1702969481000},"page":"15473-15489","source":"Crossref","is-referenced-by-count":0,"title":["Evaluation of methods to determine the surface mixing layer height of the atmospheric boundary layer in the central Arctic during polar night and transition to polar day in cloudless and cloudy conditions"],"prefix":"10.5194","volume":"23","author":[{"ORCID":"http:\/\/orcid.org\/0000-0002-5869-5752","authenticated-orcid":false,"given":"Elisa F.","family":"Akansu","sequence":"first","affiliation":[]},{"ORCID":"http:\/\/orcid.org\/0000-0002-0395-9597","authenticated-orcid":false,"given":"Sandro","family":"Dahlke","sequence":"additional","affiliation":[]},{"given":"Holger","family":"Siebert","sequence":"additional","affiliation":[]},{"ORCID":"http:\/\/orcid.org\/0000-0002-4652-5561","authenticated-orcid":false,"given":"Manfred","family":"Wendisch","sequence":"additional","affiliation":[]}],"member":"3145","published-online":{"date-parts":[[2023,12,19]]},"reference":[{"key":"ref1","doi-asserted-by":"crossref","unstructured":"Achtert, P., Brooks, I. M., Brooks, B. J., Moat, B. I., Prytherch, J., Persson, P. O. G., and Tjernstr\u00f6m, M.: Measurement of wind profiles by motion-stabilised ship-borne Doppler lidar, Atmos. Meas. Tech., 8, 4993\u20135007, https:\/\/doi.org\/10.5194\/amt-8-4993-2015, 2015.\u2002a","DOI":"10.5194\/amt-8-4993-2015"},{"key":"ref2","doi-asserted-by":"crossref","unstructured":"Akansu, E.\u00a0F., Siebert, H., Dahlke, S., Graeser, J., Jaiser, R., and Sommerfeld, A.: Tethered balloon-borne measurements of turbulence during the MOSAiC expedition from December 2019 to May 2020, PANGAEA [data set], https:\/\/doi.org\/10.1
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