دورية أكاديمية

A systematic assessment of water vapor products in the Arctic: from instantaneous measurements to monthly means

التفاصيل البيبلوغرافية
العنوان: A systematic assessment of water vapor products in the Arctic: from instantaneous measurements to monthly means
المؤلفون: S. Crewell, K. Ebell, P. Konjari, M. Mech, T. Nomokonova, A. Radovan, D. Strack, A. M. Triana-Gómez, S. Noël, R. Scarlat, G. Spreen, M. Maturilli, A. Rinke, I. Gorodetskaya, C. Viceto, T. August, M. Schröder
المصدر: Atmospheric Measurement Techniques, Vol 14, Pp 4829-4856 (2021)
بيانات النشر: Copernicus Publications, 2021.
سنة النشر: 2021
المجموعة: LCC:Environmental engineering
LCC:Earthwork. Foundations
مصطلحات موضوعية: Environmental engineering, TA170-171, Earthwork. Foundations, TA715-787
الوصف: Water vapor is an important component in the water and energy cycle of the Arctic. Especially in light of Arctic amplification, changes in water vapor are of high interest but are difficult to observe due to the data sparsity of the region. The ACLOUD/PASCAL campaigns performed in May/June 2017 in the Arctic North Atlantic sector offers the opportunity to investigate the quality of various satellite and reanalysis products. Compared to reference measurements at R/V Polarstern frozen into the ice (around 82∘ N, 10∘ E) and at Ny-Ålesund, the integrated water vapor (IWV) from Infrared Atmospheric Sounding Interferometer (IASI) L2PPFv6 shows the best performance among all satellite products. Using all radiosonde stations within the region indicates some differences that might relate to different radiosonde types used. Atmospheric river events can cause rapid IWV changes by more than a factor of 2 in the Arctic. Despite the relatively dense sampling by polar-orbiting satellites, daily means can deviate by up to 50 % due to strong spatio-temporal IWV variability. For monthly mean values, this weather-induced variability cancels out, but systematic differences dominate, which particularly appear over different surface types, e.g., ocean and sea ice. In the data-sparse central Arctic north of 84∘ N, strong differences of 30 % in IWV monthly means between satellite products occur in the month of June, which likely result from the difficulties in considering the complex and changing surface characteristics of the melting ice within the retrieval algorithms. There is hope that the detailed surface characterization performed as part of the recently finished Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) will foster the improvement of future retrieval algorithms.
نوع الوثيقة: article
وصف الملف: electronic resource
اللغة: English
تدمد: 1867-1381
1867-8548
Relation: https://amt.copernicus.org/articles/14/4829/2021/amt-14-4829-2021.pdf; https://doaj.org/toc/1867-1381; https://doaj.org/toc/1867-8548
DOI: 10.5194/amt-14-4829-2021
URL الوصول: https://doaj.org/article/daa1e179976c4eac8cf6bbd12d4dd6ca
رقم الأكسشن: edsdoj.1e179976c4eac8cf6bbd12d4dd6ca
قاعدة البيانات: Directory of Open Access Journals
الوصف
تدمد:18671381
18678548
DOI:10.5194/amt-14-4829-2021