Precipitation over the Southern Ocean: properties and formation mechanisms

Bibliographic Details
Main Author: Luís, Diogo da Silva
Publication Date: 2022
Format: Master thesis
Language: eng
Source: Repositórios Científicos de Acesso Aberto de Portugal (RCAAP)
Download full: http://hdl.handle.net/10773/38656
Summary: Uncertainty in Southern Ocean/Antarctica precipitation estimates is high due to the lack of measurements to evaluate model and reanalysis products performance. Unique precipitation measurements were carried out during the Swiss Polar Institute’s Antarctic Circumnavigation Expedition (ACE) (December 2016 - March 2017). High temporal resolution measurements of precipitation were performed by a Snow Particle Counter (SPC) and by a Micro Rain Radar (MRR) aboard the RV Akademik Tryoshnikov. Radiosondes were launched periodically to observe the vertical structure of the atmosphere. Additionally, MRR and radiosonde measurements from Dumont D’Urville station (DDU) were available when the expedition was in the Mertz Glacier region. In this work, the snowfall observed during ACE was analysed. Two distinct snowfall events that occurred during the ACE campaign were chosen to evaluate ECMWF’s ERA5 reanalysis product and AMPS (Antarctic Mesoscale Prediction System using Polar-WRF model). The first event on 2 February 2017 was associated with an extratropical cyclone east of Adélie Land and a moderate along-shore moisture transport. The second event on 8-10 February 2017 was associated with a cyclone west of Mertz blocked by a high-pressure ridge, directing a strong moisture transport (classified as an atmospheric river) towards Adélie Land with precipitation affecting the coastal region. The precipitation amount and phase, as well as vertical profiles, are analysed using observations, and compared to the model and reanalysis data.
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spelling Precipitation over the Southern Ocean: properties and formation mechanismsAntarcticaSouthern OceanPrecipitationUncertainty in Southern Ocean/Antarctica precipitation estimates is high due to the lack of measurements to evaluate model and reanalysis products performance. Unique precipitation measurements were carried out during the Swiss Polar Institute’s Antarctic Circumnavigation Expedition (ACE) (December 2016 - March 2017). High temporal resolution measurements of precipitation were performed by a Snow Particle Counter (SPC) and by a Micro Rain Radar (MRR) aboard the RV Akademik Tryoshnikov. Radiosondes were launched periodically to observe the vertical structure of the atmosphere. Additionally, MRR and radiosonde measurements from Dumont D’Urville station (DDU) were available when the expedition was in the Mertz Glacier region. In this work, the snowfall observed during ACE was analysed. Two distinct snowfall events that occurred during the ACE campaign were chosen to evaluate ECMWF’s ERA5 reanalysis product and AMPS (Antarctic Mesoscale Prediction System using Polar-WRF model). The first event on 2 February 2017 was associated with an extratropical cyclone east of Adélie Land and a moderate along-shore moisture transport. The second event on 8-10 February 2017 was associated with a cyclone west of Mertz blocked by a high-pressure ridge, directing a strong moisture transport (classified as an atmospheric river) towards Adélie Land with precipitation affecting the coastal region. The precipitation amount and phase, as well as vertical profiles, are analysed using observations, and compared to the model and reanalysis data.A incerteza nas estimativas de precipitação no Oceano Antártico/Antártica é alta devido à falta de medições para avaliar o desempenho dos modelos e de produtos de reanálise. Medições únicas de precipitação foram realizadas durante a Expedição de Circum-Navegação Antártica (ACE) do Instituto Polar Suíço (dezembro de 2016 a março de 2017). Medições de precipitação com alta resolução temporal foram realizadas por um Snow Particle Counter (SPC) e por um Micro Rain Radar (MRR) a bordo do RV Akademik Tryoshnikov. Radiossondas foram lançadas periodicamente para observar a estrutura vertical da atmosfera. Além disso, medições de MRR e radiossondagens da estação Dumont D’Urville (DDU) foram usadas quando a expedição estava na região do Glaciar Mertz. Neste trabalho, foi analisada a queda de neve observada durante a ACE. Dois eventos distintos de queda de neve que ocorreram durante a campanha ACE foram escolhidos para avaliar as reanálises ERA5 do ECMWF e o modelo AMPS Polar-WRF. O primeiro evento, em 2 de fevereiro de 2017, esteve associado a um ciclone extratropical a leste de Adélie Land e a um transporte moderado de humidade ao longo da costa. O segundo evento, de 8 a 10 de fevereiro de 2017, esteve associado a um ciclone a oeste de Mertz que foi bloqueado por um anticiclone, que direcionou um forte transporte de humidade (classificado como rio atmosférico) para Adélie Land com precipitação a afetar a região costeira. A quantidade e a fase da precipitação, bem como os perfis verticais, foram analisados usando observações e comparados com dados de modelo e de reanálises.2023-07-14T10:32:42Z2022-12-06T00:00:00Z2022-12-06info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/masterThesisapplication/pdfhttp://hdl.handle.net/10773/38656engLuís, Diogo da Silvainfo:eu-repo/semantics/openAccessreponame:Repositórios Científicos de Acesso Aberto de Portugal (RCAAP)instname:FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologiainstacron:RCAAP2024-05-06T04:47:29Zoai:ria.ua.pt:10773/38656Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireinfo@rcaap.ptopendoar:https://opendoar.ac.uk/repository/71602025-05-28T14:20:26.642602Repositórios Científicos de Acesso Aberto de Portugal (RCAAP) - FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologiafalse
dc.title.none.fl_str_mv Precipitation over the Southern Ocean: properties and formation mechanisms
title Precipitation over the Southern Ocean: properties and formation mechanisms
spellingShingle Precipitation over the Southern Ocean: properties and formation mechanisms
Luís, Diogo da Silva
Antarctica
Southern Ocean
Precipitation
title_short Precipitation over the Southern Ocean: properties and formation mechanisms
title_full Precipitation over the Southern Ocean: properties and formation mechanisms
title_fullStr Precipitation over the Southern Ocean: properties and formation mechanisms
title_full_unstemmed Precipitation over the Southern Ocean: properties and formation mechanisms
title_sort Precipitation over the Southern Ocean: properties and formation mechanisms
author Luís, Diogo da Silva
author_facet Luís, Diogo da Silva
author_role author
dc.contributor.author.fl_str_mv Luís, Diogo da Silva
dc.subject.por.fl_str_mv Antarctica
Southern Ocean
Precipitation
topic Antarctica
Southern Ocean
Precipitation
description Uncertainty in Southern Ocean/Antarctica precipitation estimates is high due to the lack of measurements to evaluate model and reanalysis products performance. Unique precipitation measurements were carried out during the Swiss Polar Institute’s Antarctic Circumnavigation Expedition (ACE) (December 2016 - March 2017). High temporal resolution measurements of precipitation were performed by a Snow Particle Counter (SPC) and by a Micro Rain Radar (MRR) aboard the RV Akademik Tryoshnikov. Radiosondes were launched periodically to observe the vertical structure of the atmosphere. Additionally, MRR and radiosonde measurements from Dumont D’Urville station (DDU) were available when the expedition was in the Mertz Glacier region. In this work, the snowfall observed during ACE was analysed. Two distinct snowfall events that occurred during the ACE campaign were chosen to evaluate ECMWF’s ERA5 reanalysis product and AMPS (Antarctic Mesoscale Prediction System using Polar-WRF model). The first event on 2 February 2017 was associated with an extratropical cyclone east of Adélie Land and a moderate along-shore moisture transport. The second event on 8-10 February 2017 was associated with a cyclone west of Mertz blocked by a high-pressure ridge, directing a strong moisture transport (classified as an atmospheric river) towards Adélie Land with precipitation affecting the coastal region. The precipitation amount and phase, as well as vertical profiles, are analysed using observations, and compared to the model and reanalysis data.
publishDate 2022
dc.date.none.fl_str_mv 2022-12-06T00:00:00Z
2022-12-06
2023-07-14T10:32:42Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/masterThesis
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