last try updating publications

Author: ecfine

_bibliography/papers.bib

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+Automatically generated by Mendeley Desktop 1.19.8
+Any changes to this file will be lost if it is regenerated by Mendeley.
 
-@string{aps = {American Physical Society,}}
+BibTeX export options can be customized via Preferences -> BibTeX in Mendeley Desktop
 
-@article{einstein1950meaning,
-  abbr={AJP},
-  bibtex_show={true},
-  title={The meaning of relativity},
-  author={Einstein, Albert and Taub, AH},
-  journal={American Journal of Physics,},
-  volume={18},
-  number={6},
-  pages={403--404},
-  year={1950},
-  publisher={American Association of Physics Teachers,}
+@misc{Finea,
+author = {Fine, Elizabeth C and Cole, Sylvia T},
+file = {:Users/ecfine/Documents/references/Mendeley/Fine, Cole/Fine, Cole{\_}Unknown{\_}Decadal observations of internal wave energy, shear, and mixing in the western Arctic Ocean.pdf:pdf},
+pages = {1--26},
+publisher = {submitted},
+title = {{Decadal observations of internal wave energy, shear, and mixing in the western Arctic Ocean}}
 }
-
-@article{PhysRev.47.777,
-  abbr={PhysRev},
-  title={Can Quantum-Mechanical Description of Physical Reality Be Considered Complete?},
-  author={Einstein, A. and Podolsky, B. and Rosen, N.},
-  abstract={In a complete theory there is an element corresponding to each element of reality. A sufficient condition for the reality of a physical quantity is the possibility of predicting it with certainty, without disturbing the system. In quantum mechanics in the case of two physical quantities described by non-commuting operators, the knowledge of one precludes the knowledge of the other. Then either (1) the description of reality given by the wave function in quantum mechanics is not complete or (2) these two quantities cannot have simultaneous reality. Consideration of the problem of making predictions concerning a system on the basis of measurements made on another system that had previously interacted with it leads to the result that if (1) is false then (2) is also false. One is thus led to conclude that the description of reality as given by a wave function is not complete.},
-  journal={Phys. Rev.,},
-  volume={47},
-  issue={10},
-  pages={777--780},
-  numpages={0},
-  year={1935},
-  month={May},
-  publisher=aps,
-  doi={10.1103/PhysRev.47.777},
-  url={http://link.aps.org/doi/10.1103/PhysRev.47.777},
-  html={https://journals.aps.org/pr/abstract/10.1103/PhysRev.47.777},
-  pdf={example_pdf.pdf},
-  selected={true}
+@misc{Fine,
+author = {Fine, Elizabeth C and Mackinnon, Jennifer A and Alford, Matthew H and Middleton, Leo and Taylor, John R. and Mickett, John B. and Cole, Sylvia T. and Couto, Nicole and {Le Boyer}, Arnaud and Peacock, Thomas},
+booktitle = {Journal of Physical Oceanography},
+file = {:Users/ecfine/Documents/references/Mendeley/Fine et al/Fine et al.{\_}Unknown{\_}Double diffusion , shear instabilities , and heat impacts of a Pacific Summer Water intrusion in the Beaufort Sea.pdf:pdf},
+publisher = {in revision},
+title = {{Double diffusion , shear instabilities , and heat impacts of a Pacific Summer Water intrusion in the Beaufort Sea}}
 }
-
-@article{einstein1905molekularkinetischen,
-  title={{\"U}ber die von der molekularkinetischen Theorie der W{\"a}rme geforderte Bewegung von in ruhenden Fl{\"u}ssigkeiten suspendierten Teilchen},
-  author={Einstein, A.},
-  journal={Annalen der physik,},
-  volume={322},
-  number={8},
-  pages={549--560},
-  year={1905},
-  publisher={Wiley Online Library}
+@article{Middleton2021b,
+author = {Middleton, L. and Fine, E. C. and MacKinnon, J. A. and Alford, M. H. and Taylor, J.R.},
+doi = {10.1029/2021gl092779},
+file = {:Users/ecfine/Documents/references/Mendeley/Middleton et al/Middleton et al.{\_}2021{\_}Estimating Dissipation Rates Associated with Double Diffusion(2).pdf:pdf},
+issn = {0094-8276},
+journal = {Geophysical Research Letters},
+pages = {1--13},
+title = {{Estimating Dissipation Rates Associated with Double Diffusion}},
+year = {2021}
 }
-
-@article{einstein1905movement,
-  abbr={Ann. Phys.},
-  title={Un the movement of small particles suspended in statiunary liquids required by the molecular-kinetic theory 0f heat},
-  author={Einstein, A.},
-  journal={Ann. Phys.,},
-  volume={17},
-  pages={549--560},
-  year={1905}
+@article{Mackinnon2016,
+abstract = {Upper-ocean turbulent heat fluxes in the Bay of Bengal and the Arctic Ocean drive regional monsoons and sea ice melt, respectively, important issues of societal interest. In both cases, accurate prediction of these heat transports depends on proper representation of the small-scale structure of vertical stratification, which in turn is created by a host of complex submesoscale processes. Though half a world apart and having dramatically different temperatures, there are surprising similarities between the two: both have (1) very fresh surface layers that are largely decoupled from the ocean below by a sharp halocline barrier, (2) evidence of interleaving lateral and vertical gradients that set upper-ocean stratification, and (3) vertical turbulent heat fluxes within the upper ocean that respond sensitively to these structures. However, there are clear differences in each ocean's horizontal scales of variability, suggesting that despite similar background states, the sharpening and evolution of mesoscale gradients at convergence zones plays out quite differently. Here, we conduct a qualitative and statistical comparison of these two seas, with the goal of bringing to light fundamental underlying dynamics that will hopefully improve the accuracy of forecast models in both parts of the world.},
+author = {Mackinnon, Jennifer A. and Nash, Jonathan D. and Alford, Matthew H. and Lucas, Andrew J. and Mickett, John B. and Shroyer, Emily L. and Waterhouse, Amy F. and Tandon, Amit and Sengupta, Debasis and Mahadevan, Amala and Ravichandran, M. and Pinkel, Robert and Rudnick, Daniel L. and Whalen, Caitlin B. and Alberty, Marion S. and {Sree Lekha}, J. and Fine, Elizabeth C. and Chaudhuri, Dipanjan and Wagner, Gregory L.},
+doi = {10.5670/oceanog.2016.38},
+file = {:Users/ecfine/Documents/references/Mendeley/Mackinnon et al/Mackinnon et al.{\_}2016{\_}A tale of two spicy seas.pdf:pdf},
+issn = {10428275},
+journal = {Oceanography},
+number = {2},
+pages = {51--61},
+title = {{A tale of two spicy seas}},
+volume = {29},
+year = {2016}
 }
-
-@article{einstein1905electrodynamics,
-  title={On the electrodynamics of moving bodies},
-  author={Einstein, A.},
-  year={1905}
+@article{PhysRevLett.113.154101,
+author = {Xu, Minghui and Tieri, D A and Fine, E C and Thompson, James K and Holland, M J},
+doi = {10.1103/PhysRevLett.113.154101},
+journal = {Phys. Rev. Lett.},
+month = {oct},
+number = {15},
+pages = {154101},
+publisher = {American Physical Society},
+title = {{Synchronization of Two Ensembles of Atoms}},
+url = {https://link.aps.org/doi/10.1103/PhysRevLett.113.154101},
+volume = {113},
+year = {2014}
+}
+@article{AntolinezJoseAntonioA.andMendezFernandoJ.andCamusPaulaandVitousekSeanandGonzalesE.MauricioandRuggieroPeterandBarnard2015,
+abstract = {Who are some of the best and brightest scientific minds of our time},
+archivePrefix = {arXiv},
+arxivId = {arXiv:1402.6991v1},
+author = {Fine, E. C. and Bryan, F. O. and Large, W. G. and Bailey, D. A.},
+doi = {10.1002/2014JC010483},
+eprint = {arXiv:1402.6991v1},
+file = {:Users/ecfine/Documents/references/Mendeley/Antolinez, Jose Antonio A. and Mendez, Fernando J. and Camus, Paula and Vitousek, Sean and Gonzale. Mauricio and Ruggiero, Peter and Barnard/Antolinez, Jose Antonio A. and Mendez, Fernando J. and Camus, Paula and Vitousek, Sean and Gonzales, E. Mauricio and Ruggiero, Peter and.pdf:pdf},
+isbn = {2169-9356},
+issn = {21699275},
+journal = {Journal of Geophysical Research: Oceans},
+keywords = {10.1002/2014JD022023 and atmospheric river event,Potential vorticity,West Coast of the U.S,diabatic heating,precipitation,trajectory model},
+month = {may},
+number = {5},
+pages = {3211--3228},
+pmid = {23641116},
+title = {{An initial estimate of the global distribution of diurnal variation in sea surface salinity}},
+url = {http://doi.wiley.com/10.1002/2014JC010483},
+volume = {120},
+year = {2015}
+}
+@article{Boury2020,
+abstract = {Recent measurements and modeling indicate that roughly half of the Pacific-origin water exiting the Chukchi Sea shelf through Barrow Canyon forms a westward-flowing current known as the Chukchi Slope Current (CSC), yet the trajectory and fate of this current is presently unknown. In this study, through the combined use of shipboard velocity data and information from five profiling floats deployed as quasi-Lagrangian particles, we delve further into the trajectory and the fate of the CSC. During the period of observation, from early September to early October 2018, the CSC progressed far to the north into the Chukchi Borderland. The northward excursion is believed to result from the current negotiating Hanna Canyon on the Chukchi slope, consistent with potential vorticity dynamics. The volume transport of the CSC, calculated using a set of shipboard transects, decreased from approximately 2 Sv (1 Sv ≡ 106 m3 s-1 ) to near zero over a period of 4 days. This variation can be explained by a concomitant change in the wind stress curl over the Chukchi shelf from positive to negative. After turning northward, the CSC was disrupted and four of the five floats veered offshore, with one of the floats permanently leaving the current. It is hypothesized that the observed disruption was due to an anticyclonic eddy interacting with the CSC, which has been observed previously. These results demonstrate that, at times, the CSC can get entrained into the Beaufort Gyre.},
+author = {Boury, Samuel and Pickart, Robert S. and Odier, Philippe and Lin, Peigen and Li, Min and Fine, Elizabeth C. and Simmons, Harper L. and Mackinnon, Jennifer A. and Peacock, Thomas},
+doi = {10.1175/JPO-D-19-0273.1},
+file = {:Users/ecfine/Documents/references/Mendeley/Boury et al/Boury et al.{\_}2020{\_}Whither the Chukchi slope current.pdf:pdf},
+issn = {15200485},
+journal = {Journal of Physical Oceanography},
+number = {6},
+pages = {1717--1732},
+title = {{Whither the Chukchi slope current?}},
+volume = {50},
+year = {2020}
+}
+@article{Fine2021b,
+abstract = {An intrahalocline eddy was observed on the Chukchi slope in September of 2015 using both towed CTD and microstructure temperature and shear sections. The core of the eddy was 6°C, significantly warmer than the surrounding -1°C water and far exceeding typical temperatures of warm-core Arctic eddies. Microstructure sections indicated that outside of the eddy the rate of dissipation of turbulent kinetic energy $\epsilon$ was quite low [(10-9-10-9]. However, at the edges of the eddy core, e was elevated to . Three different processes were associated with elevated e. Double-diffusive steps were found at the eddy's top edge and were associated with an upward heat flux of 5 W m-2. At the bottom edge of the eddy, shear-driven mixing played a modest role, generating a heat flux of approximately 0.5 W m-2 downward. Along the sides of the eddy, density-compensated thermohaline intrusions transported heat laterally out of the eddy, with a horizontal heat flux of 2000 W m-2. Integrating these fluxes over an idealized approximation of the eddy's shape, we estimate that the net heat transport due to thermohaline intrusions along the eddy flanks was 2 GW, while the double-diffusive flux above the eddy was 0.4 GW. Shear-driven mixing at the bottom of the eddy accounted for only 0.04 GW. If these processes continued indefinitely at the same rate, the estimated life-span would be 1-2 years. Such eddies may be an important mechanism for the transport of Pacific-origin heat, freshwater, and nutrients into the Canada Basin.},
+author = {Fine, Elizabeth C. and MacKinnon, Jennifer A. and Alford, Matthew H. and Mickett, John B.},
+doi = {10.1175/JPO-D-18-0028.1},
+file = {:Users/ecfine/Documents/references/Mendeley/Fine et al/Fine et al.{\_}2018{\_}Microstructure observations of turbulent heat fluxes in a warm-core Canada Basin Eddy.pdf:pdf},
+issn = {15200485},
+journal = {Journal of Physical Oceanography},
+keywords = {Anticyclones,Arctic,Diapycnal mixing,Eddies,Mixing,Ship observations},
+number = {10},
+pages = {2397--2418},
+title = {{Microstructure observations of turbulent heat fluxes in a warm-core Canada Basin Eddy}},
+volume = {48},
+year = {2018}
+}
+@article{Fine2021,
+abstract = {In the Beaufort Sea in September of 2015, concurrent mooring and microstructure observations were used to assess dissipation rates in the vicinity of 72°35‘N, 145°1‘W. Microstructure measurements from a free-falling profiler survey showed very low [O (10-10)Wkg-1] turbulent kinetic energy dissipation rates $\epsilon$. A finescale parameterization based on both shear and strain measurements was applied to estimate the ratio of shear to strain R$\epsilon$ and $\epsilon$ at the mooring location, and a strain-based parameterization was applied to the microstructure survey (which occurred approximately 100 km away from the mooring site) for direct comparison with microstructure results. The finescale parameterization worked well, with discrepancies ranging from a factor of 1-2.5 depending on depth. The largest discrepancies occurred at depths with high shear. Mean R$\epsilon$ was 17, and R$\epsilon$ showed high variability with values ranging from 3 to 50 over 8 days. Observed $\epsilon$ was slightly elevated (factor of 2-3 compared with a later survey of 11 profiles taken over 3 h) from 25 to 125m following a wind event which occurred at the beginning of the mooring deployment, reaching a maximum of $\epsilon$= 6 × 10-10Wkg-1 at 30-m depth. Velocity signals associated with near-inertial waves (NIWs) were observed at depths greater than 200 m, where the Atlantic Water mass represents a reservoir of oceanic heat. However, no evidence of elevated $\epsilon$ or heat fluxes was observed in association with NIWs at these depths in either the microstructure survey or the finescale parameterization estimates.},
+author = {Fine, Elizabeth C. and Alford, Matthew H. and MacKinnon, Jennifer A. and Mickett, John B.},
+doi = {10.1175/JPO-D-19-0233.1},
+file = {:Users/ecfine/Documents/references/Mendeley/Fine et al/Fine et al.{\_}2021{\_}Microstructure mixing observations and finescale parameterizations in the beaufort sea.pdf:pdf},
+issn = {15200485},
+journal = {Journal of Physical Oceanography},
+keywords = {Arctic,Diapycnal mixing,Internal waves,Ocean,Turbulence},
+number = {1},
+pages = {19--35},
+title = {{Microstructure mixing observations and finescale parameterizations in the beaufort sea}},
+volume = {51},
+year = {2021}
 }

_pages/publications.md

@@ -3,7 +3,7 @@ layout: page
 permalink: /publications/
 title: publications
 description: publications by categories in reversed chronological order. generated by jekyll-scholar.
-years: [1956, 1950, 1935, 1905]
+years: [2021, 2020, 2018, 2015, 2014]
 nav: true
 ---