ORGANISATION/COMPANYLaboratory for Ocean Physics and Satellite remote sensing
RESEARCHER PROFILERecognised Researcher (R2)Established Researcher (R3)
APPLICATION DEADLINE06/05/2020 23:00 - Europe/Brussels
LOCATIONFrance › Plouzané
TYPE OF CONTRACTTemporary
HOURS PER WEEK35
OFFER STARTING DATE03/05/2021
The Laboratory for Ocean Physics and Satellite remote sensing (LOPS) is a high profile joint research unit that gathers staff from four renowned research institutions: the French National Centre for Scientific Research (CNRS), the French Institute for the Exploitation of the Sea (IFREMER), the Institute for Sustainable Development (IRD) and Université de Bretagne Occidentale (UBO). LOPS is located within the European University Institute for Marine Studies, in Brest, Brittany, France.
LOPS is looking for an excellent postdoctoral researcher from outside France for building together innovative aplication for an independant research fellowship through the mobility programme Marie-Sklodowska Curie Actions - European Fellowships to the next call (09 September 2020). MSCA-EF are prestigious fellowships funded by the European Commission.
They offer a rare opportunity to talented scientists:the chance to set up research programmes of their own. They provide an attractive grant for 1 to 2 years including salaries (around 2500€ net per month, with social care included) and allowances for mobility, family and research.
The deadline of submission to the European commission is on 09th September 2020; details on the call for proposal MSCA-EF webpage (the date may be subject to changes due to the current COVID-19 situation) The topic and team below have been identified for welcoming you to develop your research project at LOPS and helping you to write at persuasive proposal for the European submission in September.
Air-sea coupling - turbulent fluxes - sea spray - parameterization - tropical cyclones - midlatitude storms
Context: Strong winds over the ocean introduce substantial concentration of droplets (referred to as sea spray) into the lowest layer ~ 100 m of the atmosphere (surface layer). Mechanisms include bursting air bubbles in whitecap and tearing off the wave tips (“spume drops” ; Veron, 2015). This latter mechanism occurs for winds of 10 m/s or above. Droplets with size from 2 up to 500 μm can be transported over large distances and remain in the surface layer for several days, where they can impact the heat fluxes by increasing evaporation and sensible heat transfer. They also lower the aerodynamic roughness perceived by the airflow, resulting in less wind stress by very strong winds (e.g. Andreas et al., 2015). This should directly impact both the turbulent exchanges at the surface and the thermodynamic balance of the surface layer.
It is well established that the heat and momentum exchanges at the surface, in turn, control the initiation and intensity of the tropical cyclones. Indeed, the capacity of cyclones to develop and attain their maximum potential intensity largely depends on the ratio of enthalpy to momentum transfer (e.g. Emanuel, 1995). Recent studies underline the necessity to account for the effect of the droplet layer due to sea spray in the turbulent flux parameterizations used in numerical models for tropical cyclones prediction (e.g. Bao et al., 2011). Tests made using existing parameterizations with and without sea spray showed a significantly more intense cyclone when including the sea spray effect.
Momentum exchanges also significantly impact the intensity of mid-latitude storms. However, very large uncertainties remain both on the physical content and on the magnitude of the spray effect included in current parameterizations. More specifically, the sea spray generation functions that control the droplets distribution and concentration are very poorly known. For a given wind speed, the concentration of the droplets in the size range supposed to impact the turbulent fluxes cover several orders of magnitude (Veron, 2015).
Objectives and methods: We aim to improve the representation of the sea spray and its effects (on the surface turbulent fluxes and the thermodynamics of the surface layer) in the atmospheric models used at Meteo-France. These models share their physical parameterizations and their representation of the exchanges at the surface with the research model Meso-NH, which will be used in a flexible way for sensitivity testing. Sea spray generation functions have been implemented and used in the model, but their impact on the turbulent fluxes has not been tested extensively.
The proposed work should first consist in finalizing the implementation of sea spray generation functions. As a second step, one ought to test the sensitivity of the fluxes, the intensity of tropical cyclones and mid-latitude storms based on the uncertainties of the generation function on several realistic case studies. The tests will be performed by using an atmosphere-ocean-wave coupled platform. The parameterizations of the turbulent fluxes used in the study can start from existing functions (e.g. Bao et al., 2011 ; Andreas et al., 2015) but should represent in a more comprehensive way the effect of a high concentration of droplets in the thermodynamics of the surface layer, through the microphysical exchanges and the resulting changes of the atmospheric parameters.
Andreas EL, Mahrt L, Vickers D. (2015). An improved bulk air-sea surface flux algorithm, including spray-mediated transfer. Quarterly Journal of the Royal Meteorological Society 141(687): 642–654, doi:10.1002/qj.2424
Bao, J. W., Fairall, C. W., Michelson, S. A., & Bianco, L. (2011). Parameterizations of sea-spray impact on the air–sea momentum and heat fluxes. Monthly Weather Review, 139(12), 3781-3797.
Emanuel, K. A. (1995). Sensitivity of tropical cyclones to surface exchange coefficients and a revised steady-state model incorporating eye dynamics. Journal of the Atmospheric Sciences, 52(22), 3969-3976.
Veron F. (2015). Ocean Spray. Annual Review of Fluid Mechanics 47(1): 507–538, doi:10.1146/annurev-fluid-010814-014651
This post-doc offer is meant to be supervised by two supervisors, Marie-Noëlle Bouin (CNRM/LOPS) and Jean-Luc Redelsperger (LOPS).
Marie-Noëlle Bouin is working on improving the representation of turbulent exchanges at the air-sea interface in numerical modelling, in particular by taking into account the sea-state effect. Jean-Luc Redelsperger works on developing physical schemes in atmospheric models. Both have developed a strong expertise in using km-scale or LES ocean-wave-atmosphere coupled simulation tools.
Bouin, M.-N. and Lebeaupin Brossier, C.: Surface processes in the 7 November 2014 medicane from air–sea coupled high-resolution numerical modelling, Atmos. Chem. Phys. Discuss., https://doi.org/10.5194/acp-2019-983, in review, 2019.
Sauvage, C., Lebeaupin Brossier, C., Bouin, M. N., & Ducrocq, V. (2020). Characterization of the air–sea exchange mechanisms during a Mediterranean heavy precipitation event using realistic sea state modelling. Atmospheric Chemistry & Physics, 20(3).
Redelsperger, J. L., Bouin, M. N., Pianezze, J., Garnier, V., & Marié, L. (2019). Impact of a sharp, small‐scale SST front on the marine atmospheric boundary layer on the Iroise Sea: Analysis from a hectometric simulation. Quarterly Journal of the Royal Meteorological Society, 145(725), 3692-3714.
Bourras, D., Cambra, R., Marié, L., Bouin, M. N., Baggio, L., Branger, H., ... & Maes, C (2019). Air‐Sea Turbulent Fluxes From a Wave‐Following Platform During Six Experiments at Sea. Journal of Geophysical Research: Oceans, 124(6), 4290-4321.
Bouin, M. N., Redelsperger, J. L., & Lebeaupin Brossier, C. (2017). Processes leading to deep convection and sensitivity to sea‐state representation during HyMeX IOP8 heavy precipitation event. Quarterly Journal of the Royal Meteorological Society, 143(707), 2600-2615.
This project is part of a joint effort involving several laboratories (CNRM, LACy, LOPS), to improve the overall representation of wind and turbulent fluxes in severe weather conditions. This post-doc proposal is following a first study on the sea spray impact on tropical cyclones (J. Pianezze, LACy) within the framework of the project RenovRisk that received funding from the European Regional Development Fund (ERDF). In addition, the ongoing project Caravele (R. Fernandes, LOPS) addresses the impact of wave breaking in momentum flux parameterization. This latter project is funded by the French National Research Agency (ANR). Eventually, a current PhD position (L. Corale, LACy) aims at implementing ocean-wave-atmosphere coupling in the operational numerical tools of Meteo-France for tropical cyclone forecasting.
MSCA-EF are prestigious fellowships funded by the European Commission. They offer a rare opportunity to talented scientists: the chance to set up research programmes of their own. They provide an attractive grant for 1 to 2 years including salaries and allowances for mobility, family and research.
Applicants must be «Experienced Researchers» (i.e. by the time of the MSCA deadline (09 September 2020), be in possession of a doctoral degree or have at least four years of full-time equivalent research experience).
Applicants can be of any nationality but must not have spent mor than 12 months in France in the 3 years immediately prior to MSCA deadline
We encourage all motivated post-docs to apply on EU Survey (link here), as early as possible and at least before the 6th May 2020. In your application you have to include:
- a CV including : (i) the exact date of your stay in each position and/or country and (ii) a list of publications;
- a research outline document (up to 2 pages) identifying the research synergies with the faculty members / pre-identified topics.
Following the reception of your application, we will check the eligibility of your profile for a MSCA-EF application. Then supervisor(s) will select the most promising applications regarding the excellence-based competitive conditions and evaluation criteria of the MSCA-EF program and contact them in due course (mid-May) for further discussions and proposal writing until September 2020. If funded, the project proposed in September 2020 could start from May 2021 onwards.
To be crystal clear, this is the responsibility of the fellow to develop and write his/her own application proposal, but the supervisor will be deeply involved in the co-writing of the proposal and you will also receive dedicated support from the European office to write a persuasive proposal in a continuous follow-up process.
The candidate should have a recent Ph.D. in atmospheric science or in a related discipline and preferably some experience in atmospheric mesoscale modeling.
A good understanding of the physics of turbulence and of the exchanges at the air-sea interface is requested.
Additional knowledge in tropical cyclones and/or microphysical atmospheric processes would be positively considered
EURAXESS offer ID: 509645
The responsibility for the jobs published on this website, including the job description, lies entirely with the publishing institutions. The application is handled uniquely by the employer, who is also fully responsible for the recruitment and selection processes.
Please contact email@example.com if you wish to download all jobs in XML.