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Properties of Snow Overlying the Sea Ice Off East Antarctica in Late Winter, 2007
Title Properties of snow overlying the sea ice off East Antarctica in late winter, 2007 Author(s) Toyota, Takenobu; Massom, Robert; Tateyama, Kazutaka; Tamura, Takeshi; Fraser, Alexander Deep Sea Research Part II : Topical Studies in Oceanography, 58(9-10), 1137-1148 Citation https://doi.org/10.1016/j.dsr2.2010.12.002 Issue Date 2011-05 Doc URL http://hdl.handle.net/2115/46198 Type article (author version) File Information DSR58-9-10_1137-1148.pdf Instructions for use Hokkaido University Collection of Scholarly and Academic Papers : HUSCAP Title: Properties of snow overlying the sea ice off East Antarctica in late winter, 2007 Authors: Takenobu Toyota1, Robert Massom2, Kazutaka Tateyama3, Takeshi Tamura 4, and Alexander Fraser5 Submitted to Deep Sea Research II Affiliation 1*: Institute of Low Temperature Science, Hokkaido University N19W8, Kita-ku, Sapporo, 060-0819, Japan ([email protected]) *corresponding author Tel: +81-11-706-7431 Fax: +81-11-706-7142 2: Australian Antarctic Division and Antarctic Climate and Ecosystems Cooperative Research Centre, c/o University of Tasmania, Sandy Bay, Tasmania 7001, Australia 3: Kitami Institute of Technology, Kouencho, Kitami 090-8507, Japan 4: Antarctic Climate and Ecosystems Cooperative Research Centre, c/o University of Tasmania, Sandy Bay, Tasmania 7001, Australia 5: Institute of Marine and Antarctic Studies, Antarctic Climate and Ecosystems Cooperative Research Centre, University of Tasmania, Sandy Bay, Tasmania 7001, Australia 1 Abstract The properties of snow on East Antarctic sea ice off Wilkes Land were examined during the Sea Ice Physics and Ecosystem Experiment (SIPEX) in late winter of 2007, focusing on the interaction with sea ice. -
Advances in Tropical Cyclone Research
PART 5 Advances in Tropical Cyclone Research 21 Introduction to Hurricane Dynamics: Tropical Cyclone Intensification Michael T. Montgomery Department of Meteorology, Naval Postgraduate School Monterey, California, USA [email protected] 1. Introduction The broad aim of this set of two articles on tropical cyclone theory is to provide graduate students and post-doctoral researchers from India and other parts of the world with state-of-the-art knowledge and understanding of tropical cyclone dynamics. It is hoped that this knowledge base will be a useful tool to help these students and post docs understand and improve the forecasts of tropical cyclone genesis and intensification in various parts of the world affected by these storms. To me, tropical cyclones are magnificent and scientifically fascinating large-scale convective vortices that still hold many hidden secrets regarding their birth, intensification, mature evolution and decay. Observing the formation and intensification of these large-scale coherent structures fuels my scientific passion to obtain a deeper physical understanding of what many atmospheric scientists have called “the greatest storms on earth” (see examples in Fig. 1). Practical considerations, such as saving human life and property in the path of these tropical tempests are, of course, another important driving factor in the quest for knowledge about these storms. My interest in these storms spans all facets of these storms. Recent events surrounding Hurricane Sandy (2012) are a reminder that even tropical storms can wreak havoc on populated coastal communities, maritime assets and even inland populations (e.g., Lussier et al., 2015). As coastal communities continue to grow, there is an increasing demand throughout regions of the world for more accurate tropical cyclone forecasts. -
Laboratory Study of Initial Sea-Ice Growth: Properties of Grease Ice and Nilas
The Cryosphere, 6, 729–741, 2012 www.the-cryosphere.net/6/729/2012/ The Cryosphere doi:10.5194/tc-6-729-2012 © Author(s) 2012. CC Attribution 3.0 License. Laboratory study of initial sea-ice growth: properties of grease ice and nilas A. K. Naumann1, D. Notz1, L. Havik˚ 2, and A. Sirevaag2 1Max Planck Institute for Meteorology, Hamburg, Germany 2Geophysical Institute, University of Bergen, Bergen, Norway Correspondence to: A. K. Naumann ([email protected]) Received: 23 December 2011 – Published in The Cryosphere Discuss.: 13 January 2012 Revised: 26 May 2012 – Accepted: 12 June 2012 – Published: 10 July 2012 Abstract. We investigate initial sea-ice growth in an ice-tank parts of the water surface ice free and therefore allowed for a study by freezing an NaCl solution of about 29 g kg−1 in higher heat loss from the water. The development of the ice three different setups: grease ice grew in experiments with thickness can be reproduced well with simple, one dimen- waves and in experiments with a current and wind, while ni- sional models that only require air temperature or ice surface las formed in a quiescent experimental setup. In this paper temperature as input. we focus on the differences in bulk salinity, solid fraction and thickness between these two ice types. The bulk salinity of the grease-ice layer in our experiments remained almost constant until the ice began to consolidate. 1 Introduction In contrast, the initial bulk-salinity evolution of the nilas is well described by a linear decrease of about 2.1 g kg−1 h−1 Sea-ice growth in turbulent water differs from sea-ice growth independent of air temperature. -
Suivi Sismologique De L'impact Des Cyclones Sur La Charge De Fond De
Université de La Réunion – Laboratoire Géosciences Réunion – IPGP THÈSE Pour obtenir le grade de DOCTEUR D’UNIVERSITÉ Spécialité : Sismologie Par Alicia GONZALEZ Suivi sismologique de l’impact des cyclones sur la charge de fond de la Rivière des Pluies et de la Rivière du Mât à La Réunion Soutenue publiquement le 28 juin 2019, devant le jury composé de : Christel TIBERI Chargée de Recherche, Université de Montpellier Rapporteure Eric LAROSE Directeur de Recherche, ISTerre Grenoble Rapporteur Florent GIMBERT Chargé de Recherche, IGE Grenoble Examinateur Alain RECKING Chargé de Recherche, IRSTEA Grenoble Examinateur Jean-Lambert JOIN Professeur, Université de La Réunion Examinateur Fabrice R. FONTAINE Maitre de Conférence, Université de La Réunion Directeur Guilhem BARRUOL Directeur de Recherche, IPGP Co-Directeur Valérie FERRAZZINI Directeur de Recherche, IPGP Invitée Avant-propos Thèse réalisée au Laboratoire Géosciences Reunion (LGSR) bât. S1 15 Av. René Cassin CS 92003 97744 Saint-Denis Tél. : 0262938211 Web : https://geosciences.univ-reunion.fr/home Sous la direction de Fabrice Fontaine [email protected] et la co-direction de Guilhem Barruol [email protected] Financement Allocation sans contrat : soutien financier de la Région Réunion et de l’Union Européenne – Fonds européen de développement régional (FEDER) PO 2014-2020. Remerciements Ma première pensée va à Fabrice Fontaine, mon directeur de thèse, qui a eu confiance en mes capacités pour relever ce challenge. Fabrice, je te serai à jamais reconnaissante pour cette expérience unique. Je remercie ensuite mon co-directeur de thèse Guilhem Barruol pour son encadrement depuis Paris. Merci pour les nombreux conseils, corrections, propositions, les discussions essentielles qui m'ont souvent redonné confiance en mes raisonnements, merci de m'avoir accueilli à Paris dans une phase cruciale de production. -
Minnesota Weathertalk Newsletter for Friday, January 3, 2014
Minnesota WeatherTalk Newsletter for Friday, January 3, 2014 To: MPR's Morning Edition From: Mark Seeley, Univ. of Minnesota, Dept of Soil, Water, and Climate Subject: Minnesota WeatherTalk Newsletter for Friday, January 3, 2014 HEADLINES -December 2013 was climate near historic for northern communities -Cold start to 2014 -Weekly Weather potpourri -MPR listener questions -Almanac for January 3rd -Past weather -Outlook Topic: December 2013 near historic for far north In assessing the climate for December 2013 it should be said that from the standpoint of cold temperatures the month was quite historic for many northern Minnesota communities, especially due to the Arctic cold that prevailed over the last few days of the month. Minnesota reported the coldest temperature in the 48 contiguous states thirteen times during the month, the highest frequency among all 48 states. Many northern observers saw overnight temperatures drop below -30 degrees F on several occasions. The mean monthly temperature for December from several communities ranked among the coldest Decembers ever. A sample listing includes: -4.1 F at International Falls, 2nd coldest all-time 4.6 F at Duluth, 8th coldest all-time 0.1 F at Crookston, 3rd coldest all-time -3.1 F at Roseau, 3rd coldest all-time 0.3 F at Park Rapids, 3rd coldest all-time -4.4 F at Embarrass, 2nd coldest all-time -4.1 F at Baudette, coldest all-time -3.7 F at Warroad, coldest all-time -2.9 F at Babbitt, coldest all-time -2.8 F at Gunflint Lake, coldest all-time In addition, some communities reported an exceptionally snowy month of December. -
Short Curriculum Vitae
Prof. Virginie K.E. DUVAT UMR LIENSs 7266 - Littoral, Environment and Societies La Rochelle University-CNRS (National Centre for Scientific Research) Institute of Littoral and Environment, 2 rue Olympe de Gouges- 17000 La Rochelle - France Email: [email protected] Tel Office: + 33 5 46 50 76 47 / Mobile: + 33 6 50 81 39 27 SHORT CURRICULUM VITAE 1. Professional experience and position Since 2006 Professor in Coastal Geography, La Rochelle University, La Rochelle, France 1999-2006 Assistant Professor in Coastal Geography, University of La Reunion (south-western Indian Ocean), France 2. Education 2005 Accreditation to supervise research (HDR in French) in Geography, University of Paris IV-Sorbonne, France - Title: Geomorphology and management of coral beaches in south-western Indian Ocean Islands (in French). 1996-1998 PhD in Coastal Geography, University of Reunion Island, France – Title: Coral beaches and islands of the Seychelles Islands: from physical processes to beach and island management (Mahe, Praslin, La Digue and Desroches islands) – award of the French Geographical Society (Paris) for my PhD thesis 3. Fields of expertise 3.1. Thematic areas: è Coastal geomorphology: 1950s-Present changes in the configuration of atoll reef islands and high mountainous islands’ beach-dune systems, including island and shoreline change assessment, impacts of and resilience to tropical cyclones (including marine inundation and river flooding, impacts on shoreline position and on coastal vegetation), interference of human activities with natural processes, island-reef ecosystem interactions – See for example: Duvat et al., 2016; Testut, Duvat et al., 2016; Duvat and Pillet, 2017; Duvat et al., 2017; Duvat et al., 2017; Collin, Duvat et al., 2021. -
R&R 2019 GB.Indd
12 n=1 LG Kelvin 3 days 12 12 6 days n=1 ER 30 days Research Report 2018 Research Report 2018 Table of contents Numerical weather prediction and data assimilations page 5 Process studies page 14 Climate page 22 Diagnostic, study and climate modelling, from season to century Impacts and adaptation Chemistry, aerosols and air quality page 34 Snow page 38 Oceanography page 41 Engineering, campaigns and observation products page 46 Observation engineering and products Campaigns Research and aeronautics page 54 Appendix page 59 Numerical weather prediction and data assimilations Meteo-France operates several state-of-the-art operational numerical weather prediction systems: a global one called ARPEGE and a convection-permitting one called AROME. AROME is run on many limited areas around the Globe, the instance covering mainland France (AROME-F) further benefits from a 3D variational data assimilation and it also provides ensemble forecasts. ARPEGE is run from 4D variational assimilations and also has both an ensemble of data assimilation as well as an ensemble forecast. Some of the most significant operational achievements of 2018 are the following ones: • The forecast range of AROME-F has been extended so as to cover the current day and the next one and the ensemble version is run 4 times/ day instead of 2. This prepares for extending the « vigilance » or public warning procedure from one to two days. • Forecasts from the overseas AROME areas all have a length of +42h. Significantly, they can be extended up to +78h if the situation requires it, which is when a tropical cyclone is threatening that area. -
A Model for Entrainment of Sediment Into Sea Ice by Aggregation Between Frazil-Ice Crystals and Sediment Grains
Journal of Glaciology, Vo l. 48, No.160, 2002 A model for entrainment of sediment into sea ice by aggregation between frazil-ice crystals and sediment grains Lars Henrik SMEDSRUD Geophysical Institute, University of Bergen, Allegaten 70,N-5007 Bergen, Norway E-mail:[email protected] ABSTRACT. Avertical numerical model has been developed that simulates tank experi- ments of sediment entrainment into sea ice. Physical processes considered were:turbulent vertical diffusion of heat, salt, sediment, frazil ice and their aggregates; differential growth of frazil-ice crystals; secondary nucleation of crystals; and aggregation between sediment and ice. The model approximated the real size distribution of frazil ice and sediment using five classes of each. Frazil crystals (25 mm to 1.5 cm) were modelled as discs with a constant 1 thickness of 30 their diameter. Each class had a constant rise velocity based on the density of ice and drag forces. Sediment grains (1^600 mm) were modelled as constant density spheres, with corresponding sinking velocities. The vertical diffusion was set constant for experi- ments based on calculated turbulent rms velocities and dissipation rates from current data. The balance between the rise/sinking velocities and the constant vertical diffusion is an im- portant feature of the model. The efficiency of the modeled entrainment process was esti- mated through , an aggregation factor. Values for are in the range h0.0003, 0.1i,but average values are often close to 0.01. Entrainment increases with increasing sediment con- centration and turbulence of the water, and heat flux to the air. 1. INTRODUCTION some experiments were completed in a larger tank at a scale more likely to represent natural conditions in time and Sediment-laden sea ice was observed during the first journey space (Smedsrud,1998, 2001; Haas and others,1999). -
ADEOS-II User's Handbook
ADEOS-II - Advanced Earth Observing Satellite-II - Reference Handbook Introduction Chapter 1 ADEOS-II Science Research Plan 1. Targets and objectives............................................................................................ 1 1.1 Targets..................................................................................................................... 1 1.2 Objectives ............................................................................................................... 2 2. Aeronomy .............................................................................................................. 3 2.1 Aeronomy with ADEOS-II..................................................................................... 3 2.2 Investigation into water cycle involving clouds ..................................................... 4 2.3 Investigation into influence on aerosols ................................................................. 5 2.4 Investigation into aeronomy in the polar regions ................................................... 5 3. Oceanography ........................................................................................................ 6 3.1 Oceanography with ADEOS-II............................................................................... 6 3.2 Marine metrology and physical oceanography....................................................... 7 3.2.1 Sea surface fluxes measurement using the satellite ....................................... 7 3.2.2 Investigation into ocean circulation mechanism........................................... -
Renovrisk: a Multidisciplinary Programme to Study the Cyclonic Risks in the South‑West Indian Ocean
Natural Hazards https://doi.org/10.1007/s11069-021-04624-w ORIGINAL PAPER ReNovRisk: a multidisciplinary programme to study the cyclonic risks in the South‑West Indian Ocean Pierre Tulet1 · Bertrand Aunay2 · Guilhem Barruol3,4 · Christelle Barthe1 · Remi Belon2 · Soline Bielli1 · François Bonnardot5 · Olivier Bousquet1 · Jean‑Pierre Cammas1,6 · Julien Cattiaux7 · Fabrice Chauvin7 · Idriss Fontaine8 · Fabrice R. Fontaine3,9 · Franck Gabarrot6 · Sabine Garabedian8 · Alicia Gonzalez3,4 · Jean‑Lambert Join3 · Florian Jouvenot10 · David Nortes‑Martinez8 · Dominique Mékiès1 · Pascal Mouquet10 · Guillaume Payen6 · Gwenaelle Pennober10 · Joris Pianezze1 · Claire Rault2 · Christophe Revillion10 · Elisa J. Rindraharisaona3,4 · Kevin Samyn2 · Callum Thompson1 · Hélène Vérèmes1,6 Received: 13 October 2020 / Accepted: 3 February 2021 © The Author(s) 2021 Abstract Today, resilience in the face of cyclone risks has become a crucial issue for our societies. With climate change, the risk of strong cyclones occurring is expected to intensify sig- nifcantly and to impact the way of life in many countries. To meet some of the associated challenges, the interdisciplinary ReNovRisk programme aims to study tropical cyclones and their impacts on the South-West Indian Ocean basin. This article is a presentation of the ReNovRisk programme, which is divided into four areas: study of cyclonic hazards, study of erosion and solid transport processes, study of water transfer and swell impacts on the coast, and studies of socio-economic impacts. The frst transdisciplinary results of the programme are presented together with the database, which will be open access from mid-2021. Keywords Tropical cyclone · Cyclonic hazards · Interdisciplinary programme · Indian Ocean 1 Introduction The South-West Indian Ocean (SWIO) is the second-to-third most active tropical cyclone basin in the world. -
ASPECT: Antarctic Sea Ice Processes & Climate
ASPeCt Antarctic Sea-Ice Processes and Climate Science and Implementation Plan 1998-2008 TABLE OF CONTENTS EXECUTIVE SUMMARY 1. OVERVIEW 1.1 Introduction 1.2 History of the ASPeCt Programme 1.3 Rationale 1.4 Overall Objectives of ASPeCt 2. KEY SCIENTIFIC QUESTIONS FOR ASPeCt 3. IMPLEMENTATION STRATEGY 3.1 Climatology 3.1.1. Reconstruction of 1980-1997 Climatology 3.1.2. Climatology Studies in the Implementation Period 1998-2008 3.1.2.1. Snow and ice thickness distributions 3.1.2.2. Snow and ice properties surveys 3.2 Process Studies 3.2.1. Short Time Series Experiments 3.2.2. Coastal Polynyas 3.2.3. Long Time Series Experiments 3.2.4. Ice Edge Experiments 3.3 Long Term Observations: Landfast Ice 4. RELATED DATA SETS AND PROGRAMME COORDINATION 4.1 Satellite Data Records 4.2 World Climate Research Programme (WCRP) 4.2.1. International Programme on Antarctic Buoys (IPAB) 4.2.2. Antarctic Ice Thickness Measurement Programme (AnITMP) 4.3 International Antarctic Zone (IAnZone) 5. REFERENCES APPENDICES A. ASPeCt Science Steering Group B. ASPeCt Activities and Schedule C. Ice Observation Protocols D. Snow and Ice Properties-Survey Protocols E. Antarctic Coastal Polynas: Candidates for ASPeCt Study F. List of Acronyms and Abbreviations FIGURES EXECUTIVE SUMMARY With the growth of activities in Global Change research in the Antarctic, both by SCAR programmes and by other international programmes such as IGBP and WCRP, key deficiencies in our understanding and lack of data from the sea ice zone have been identified. Important problems remaining to be adequately covered by Antarctic sea ice research programmes include: 1. -
Seasonal and Interannual Variability of Landfast Sea Ice in Atka Bay, 2 Weddell Sea, Antarctica
1 Seasonal and interannual variability of landfast sea ice in Atka Bay, 2 Weddell Sea, Antarctica 3 Stefanie Arndt1, Mario Hoppmann1, Holger Schmithüsen1, Alexander D. Fraser2,3, Marcel Nicolaus1 4 1Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, 27570 Bremerhaven, Germany 5 2 Institute for Marine and Antarctic Studies, University of Tasmania, Hobart 7001, Tasmania, Australia 6 3Antarctic Climate & Ecosystems Cooperative Research Centre, University of Tasmania, Hobart 7001, Tasmania, Australia 7 Correspondence to: Stefanie Arndt ([email protected]) 8 Abstract. Landfast sea ice (fast ice) attached to Antarctic (near-)coastal elements is a critical component of the local physical 9 and ecological systems. Through its direct coupling with the atmosphere and ocean, fast ice properties are also a potential 10 indicator of processes related to a changing climate. However, in-situ fast-ice observations in Antarctica are extremely sparse 11 because of logistical challenges and harsh environmental conditions. Since 2010, a monitoring program observing the seasonal 12 evolution of fast ice in Atka Bay has been conducted as part of the Antarctic Fast Ice Network (AFIN). The bay is located on 13 the north-eastern edge of Ekström Ice Shelf in the eastern Weddell Sea, close to the German wintering station Neumayer III. 14 A number of sampling sites have been regularly revisited each year between annual ice formation and breakup to obtain a 15 continuous record of sea-ice and sub-ice platelet-layer thickness, as well as snow depth and freeboard across the bay. 16 Here, we present the time series of these measurements over the last nine years.