@article{hu_chai_zhang_lang_kelley_feng_liu_atwood_atwood_2019, title={Biomimetic Self-Assembly of Co-II-Seamed Hexameric Metal-Organic Nanocapsules}, volume={141}, ISSN={["0002-7863"]}, DOI={10.1021/jacs.9b02857}, abstractNote={A CoII18L6 hexameric metal-organic nanocapsule (MONC) has been prepared and characterized using biomimetic self-assembly as the synthetic methodology. Akin to the biological behavior of zinc-finger proteins' release, uptake, and electrophilic substitution of Zn2+ ions, the assembly of this novel MONC has been accomplished by employing three sequential processes: assembly of the framework, metal ion insertion, and metal exchange, resulting in the formation of the CoII18L6 hexameric MONC. In this work, inspired by the biological behavior of metalloproteins, rational control of multiple complex supramolecular self-assembly has been achieved.}, number={23}, journal={JOURNAL OF THE AMERICAN CHEMICAL SOCIETY}, author={Hu, Xiangquan and Chai, Jie and Zhang, Chen and Lang, Jinxin and Kelley, Steven P. and Feng, Sisi and Liu, Bin and Atwood, David A. and Atwood, Jerry L.}, year={2019}, month={Jun}, pages={9151–9154} }
 @article{zhang_wen_jang_2010, title={Simulating chemistry-aerosol-cloud-radiation-climate feedbacks over the continental US using the online-coupled Weather Research Forecasting Model with chemistry (WRF/Chem)}, volume={44}, number={29}, journal={Atmospheric Environment}, author={Zhang, Y. and Wen, X. Y. and Jang, C. J.}, year={2010}, pages={3568–3582} }
 @article{zhang_farkas_hale_2002, title={Precooking and cooling of skipjack tuna (Katsuwonas pelamis): A numerical simulation}, volume={35}, ISBN={0023-6438}, DOI={10.1006/fstl.2002.0912}, abstractNote={Abstract A numerical simulation of the commercial tuna precooking and cooling process was developed as an aid to improving these critical thermal processing steps. Using the finite element method, a two-dimensional model of a tuna consisting of three regions, muscle, backbone, and viscera, was developed. Results from previous research on thermal properties of skipjack tuna were applied in the model. Preprocessor software, GAMBIT 1.1, and commercial finite element software, FIDAP 8.52, were used. The model was tested via comparison with experimental data collected in a commercial processing facility and a pilot plant. Good agreement between the simulation and experimental results was obtained.}, number={7}, journal={Food Science & Technology = Lebensmittel-Wissenschaft & -Technologie}, author={Zhang, J. and Farkas, B. E. and Hale, S. A.}, year={2002}, pages={607–616} }
 @article{xie_wu_pietrafesa_zhang_2001, title={A numerical study of wave-current interaction through surface and bottom stresses: Wind-driven circulation in the South Atlantic Bight under uniform winds}, volume={106}, ISSN={["2169-9291"]}, DOI={10.1029/2000JC000292}, abstractNote={The influences of surface waves on ocean currents in the coastal waters of the South Atlantic Bight are investigated by using a coupled wave‐current modeling system. The ocean circulation model employed is the three‐dimensional Princeton Ocean Model (POM), and the wave model invoked is an improved third‐generation wave model (WAM). The coupling procedure between the POM and the WAM and the simulated coastal ocean circulation driven by uniform surface winds are presented. The simulated results show that wind waves can significantly affect coastal ocean currents not only through an enhancement of wind stress but also through a modification of bottom stress. Wave‐induced wind stress increases the magnitude of currents both at the surface and near the seabed. On the other hand, wave‐induced bottom stress weakens the currents both at the sea surface and near the seabed. Therefore the net effect of surface wind waves on currents depends on the relative importance of current modulations by wave‐induced wind stress and bottom stress. The results further indicate that at a fixed location, the relative importance of wave‐induced surface and bottom shear stresses in coastal ocean circulation depends on the surface wind field. For the constant wind cases considered in this study, the effect of wave‐induced bottom stress is more significant in along‐shore wind conditions than in cross‐shore wind conditions.}, number={C8}, journal={JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS}, author={Xie, LA and Wu, KJ and Pietrafesa, L and Zhang, C}, year={2001}, month={Aug}, pages={16841–16855} }
 @misc{qiu_anantharamaiah_xie_vaidya_zhang_2001, title={Atmospheric pressure helium plasma treatment of ultrahigh modulus polyethylene fibres}, volume={10}, number={3}, journal={Advanced Composites Letters}, author={Qiu, Y. and Anantharamaiah, N. and Xie, S. and Vaidya, N. P. and Zhang, C.}, year={2001}, pages={135–139} }
 @article{xie_pietrafesa_zhang_1999, title={Subinertial response of the Gulf Stream system to Hurricane Fran of 1996}, volume={26}, ISSN={["0094-8276"]}, DOI={10.1029/1999GL002359}, abstractNote={The evidence of subinertial‐frequency (with periods from 2 days to 2 weeks) oceanic response to Hurricane Fran of 1996 is documented. Hurricane Fran traveled northward across the Gulf Stream and then over a cool‐core trough, known as the Charleston Trough, due east of Charleston, SC and in the lee of the Charleston Bump during the period 4–5 September, 1996. During the passage of the storm, the trough closed into a gyre to form an intense cool‐core cyclonic eddy. This cool‐core eddy had an initial size of approximately 130 km by 170 km and drifted northeastward along the Gulf Stream front at a speed of 13 to 15 km/day as a subinertial baroclinic wave. Superimposed on this subinertial‐frequency wave were near‐inertial frequency, internal inertia‐gravity waves formed in the stratified mixed‐layer base after the passage of the storm. The results from a three‐dimensional numerical ocean model confirm the existence of both near‐inertial and subinertial‐frequency waves in the Gulf Stream system during and after the passage of Hurricane Fran. Model results also showed that hurricane‐forced oceanic response can modify Gulf Stream variability at both near‐inertial and subinertial frequencies.}, number={23}, journal={GEOPHYSICAL RESEARCH LETTERS}, author={Xie, L and Pietrafesa, LJ and Zhang, C}, year={1999}, month={Dec}, pages={3457–3460} }
 @article{xie_pietrafesa_bohm_zhang_li_1998, title={Evidence and mechanism of Hurricane Fran induced cooling in the Charleston trough}, volume={25}, ISSN={["0094-8276"]}, DOI={10.1029/98GL00180}, abstractNote={Evidence of enhanced sea surface cooling during and following the passage of Hurricane Fran in September 1996 over an oceanic depression located on the ocean margin offshore of Charleston, South Carolina (referred to as the Charleston Trough), [Pietrafesa, 1983] is documented. Approximately 4C° of sea surface temperature (SST) reduction within the Charleston Trough following the passage of Hurricane Fran was estimated based on SST imagery from Advanced Very High Resolution Radiometer (AVHRR) on the NOAA‐14 polar orbiting satellite. Simulations using a three‐dimensional coastal ocean model indicate that the largest SST reduction occurred within the Charleston Trough. This SST reduction can be explained by oceanic mixing due to storm‐induced internal inertia‐gravity waves.}, number={6}, journal={GEOPHYSICAL RESEARCH LETTERS}, author={Xie, L and Pietrafesa, LJ and Bohm, E and Zhang, C and Li, X}, year={1998}, month={Mar}, pages={769–772} }