دورية أكاديمية

Comparison of ozone profiles from DIAL, MLS, and chemical transport model simulations over Río Gallegos, Argentina, during the spring Antarctic vortex breakup, 2009

التفاصيل البيبلوغرافية
العنوان: Comparison of ozone profiles from DIAL, MLS, and chemical transport model simulations over Río Gallegos, Argentina, during the spring Antarctic vortex breakup, 2009
المؤلفون: Sugita, Takafumi, Akiyoshi, Hideharu, Wolfram, Elián, Salvador, Jacobo, Ohyama, Hirofumi, Mizuno, Akira
بيانات النشر: Copernicus Publications
سنة النشر: 2017
المجموعة: Niedersächsisches Online-Archiv NOA (Gottfried Wilhelm Leibniz Bibliothek Hannover)
مصطلحات موضوعية: article, Verlagsveröffentlichung
الوصف: This study evaluates the agreement between ozone profiles derived from the ground-based differential absorption lidar (DIAL), satellite-borne Aura Microwave Limb Sounder (MLS), and 3-D chemical transport model (CTM) simulations such as the Model for Interdisciplinary Research on Climate (MIROC-CTM) over the Atmospheric Observatory of Southern Patagonia (Observatorio Atmosférico de la Patagonia Austral, OAPA; 51.6° S, 69.3° W) in Río Gallegos, Argentina, from September to November 2009. In this austral spring, measurements were performed in the vicinity of the polar vortex and inside it on some occasions; they revealed the variability in the potential vorticity (PV) of measured air masses. Comparisons between DIAL and MLS were performed between 6 and 100 hPa with 500 km and 24 h coincidence criteria. The results show a good agreement between DIAL and MLS with mean differences of ±0.1 ppmv (MLS − DIAL, n = 180) between 6 and 56 hPa. MIROC-CTM also agrees with DIAL, with mean differences of ±0.3 ppmv (MIROC-CTM − DIAL, n = 23) between 10 and 56 hPa. Both comparisons provide mean differences of 0.5 ppmv (MLS) to 0.8–0.9 ppmv (MIROC-CTM) at the 83–100 hPa levels. DIAL tends to underestimate ozone values at this lower altitude region. Between 6 and 8 hPa, the MIROC-CTM ozone value is 0.4–0.6 ppmv (5–8 %) smaller than those from DIAL. Applying the scaled PV (sPV) criterion for matching pairs in the DIAL–MLS comparison, the variability in the difference decreases 21–47 % between 10 and 56 hPa. However, the mean differences are small for all pressure levels, except 6 hPa. Because ground measurement sites in the Southern Hemisphere (SH) are very sparse at mid- to high latitudes, i.e., 35–60° S, the OAPA site is important for evaluating the bias and long-term stability of satellite instruments. The good performance of this DIAL system will be useful for such purposes in the future.
نوع الوثيقة: article in journal/newspaper
وصف الملف: electronic
اللغة: English
العلاقة: Atmospheric Measurement Techniques -- http://www.bibliothek.uni-regensburg.de/ezeit/?2505596Test -- http://www.atmospheric-measurement-techniques.netTest/ -- 1867-8548; https://doi.org/10.5194/amt-10-4947-2017Test; https://noa.gwlb.de/receive/cop_mods_00007739Test; https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00007696/amt-10-4947-2017.pdfTest; https://amt.copernicus.org/articles/10/4947/2017/amt-10-4947-2017.pdfTest
DOI: 10.5194/amt-10-4947-2017
الإتاحة: https://doi.org/10.5194/amt-10-4947-2017Test
https://noa.gwlb.de/receive/cop_mods_00007739Test
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00007696/amt-10-4947-2017.pdfTest
https://amt.copernicus.org/articles/10/4947/2017/amt-10-4947-2017.pdfTest
حقوق: https://creativecommons.org/licenses/by/4.0Test/ ; uneingeschränkt ; info:eu-repo/semantics/openAccess
رقم الانضمام: edsbas.E5F8FDF2
قاعدة البيانات: BASE