The experience of remote temperature-water content sounding of atmosphere during drift of R/V “Akademik Tryoshnikov”

• Published in: Arctic and Antarctic Research
• Main Authors: A. Makshtas P., G. Il’in N., V. Bykov Yu., E. Miller A., A. Troitsky V., V. Kustov Yu., I. Bolshakova I., D. Rize D., А. Макштас П., Г. Ильин Н., В. Быков Ю., Е. Миллер А., А. Троицкий В., В. Кустов Ю., И. Большакова И., Д. Ризе Д.
• Other Authors: This work was supported by the Russian Ministry of Education and Science (project RFMEFI61619X0108)., Работа выполнена при финансовой поддержке Минобрнауки России (проект RFMEFI61619X0108).
• Format: Article in Journal/Newspaper
• Language: Russian
• Published: Государственный научный центр Российской Федерации Арктический и антарктический научно-исследовательский институт 2020
• Subjects: inversion;polar atmosphere;radiometric complex;radiosounding;remote sensing;water content; влагосодержание;дистанционное зондирование;инверсия;полярная атмосфера;радиозондирование;радиометрический комплекс; Arctic; Barentsburg; Weddell; Weddell Sea; Sea ice
• Online Access: https://www.aaresearch.science/jour/article/view/294; https://doi.org/10.30758/0555-2648-2020-66-3-349-363

For the first time experience was gained with the operation of Russian equipment for water content and temperature remote sensing of the lower atmosphere in the Arctic. The comparison the results of measurements by radiometric systems with data of radiosoundings in wide range of meteorological conditions had been executed. It is shown that mean difference between integral atmospheric water content, measured by water vapor radiometer WVR, and calculated from radiosoundings data does not exceed 6 % with standard deviation 0.54 kg/m2 and significant correlation coefficient 0,92. Analysis the data of meteorological temperature profiler MTR-5 allows to conclude that in general its adequately reproduce air temperature profiles in the atmospheric lower 1000 m layer. Some deviations take place only in cases of large temperature gradients. Preliminary analysis of WVR data showed that monthly mean value of integral atmospheric water content in area under study in April 2019 year practically coincides with calculated from radiosoundings, performed in 1983—1988 years at the polar station Barentsburg, nearest to the drift region, 3.61 and 3.62 kg/m2 respectively. Same time hourly mean values of integral atmospheric water content during drift varied from 2 to 10 kg/m2, with extreme values recorded between April 15 and April 20, probably due to intensive transport of air masses of the Atlantic origin. Based on MTR-5 data it was concluded that despite differences in sounding technology, the place and time of observations, the statistics of inversions registered during drift correspond well to statistics of inversions, recorded on the Arctic coastal stations and over sea ice cover of the Weddell Sea in winter. Приведено описание работы комплекса аппаратуры влажностно-температурного дистанционного зондирования нижнего слоя атмосферы (радиометр РВП и метеорологический профилемер МТР-5РЕ) в условиях Арктики. Выполнено сравнение результатов измерений радиометрических систем с данными аэрологического зондирования в широком спектре метеорологических условий. Получены оценки интегрального влагосодержания атмосферы и характеристик инверсий в нижнем 1000-метровом слое атмосферы в период дрейфа НЭС «Академик Трёшников» в северной части Баренцева моря.