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301. Resonance in Fast-Wave Amplitude in the Periphery of Cylindrical Plasmas and Application to Edge Losses of Wave Heating Power in Tokamaks

303. Sherlock Movie Watching Dataset

305. Supplementary Model Output to "Climate, soil organic layer, and nitrogen jointly drive forest development after fire in the North American boreal zone"

306. Three New Extreme Ultraviolet Spectrometers on NSTX-U for Impurity Monitoring

307. Time dependent analysis of visible helium line-ratios for electron temperature and density diagnostic using synthetic simulations on NSTX-U

308. Understanding the dynamics and energetics of magnetic reconnection in a laboratory plasma: Review of recent progress on selected fronts

309. Attentional Modulation of Brain Responses to Primary Appetitive and Aversive Stimuli

310. Evolution patterns and parameter regimes in edge localized modes on the National Spherical Torus Experiment

312. Basin-Scale Leakage Risks from Geologic Carbon Sequestration: Impact on Carbon Capture and Storage Energy Market Competitiveness

313. Complete Dataset for Williams Site Pore Water Chemistry, March 2011 - April 2012

314. Dataset for JGR Article (DOI: 10.1002/2014JD022278)

316. 60 degree Inclined Pulsar

317. 90 degree Inclined Pulsar

318. Aligned Nonspinning Dipoles

319. Aligned Rapidly Spinning Dipoles

320. Antialigned Nonspinning Dipoles

321. Antialigned Rapidly Spinning Dipoles

322. Dynamical Magnetic Fields of Antialigned Nonspinning Dipoles

327. A reduced-turbulence regime in the Large Helical Device upon injection of low-Z materials powders

345. Enhancement of edge turbulence concomitant with ELM suppression during boron powder injection in EAST

348. First impurity powder injection experiments in LHD

357. Lower Hybrid Drift Waves During Guide Field Reconnection

360. Nasa Budgetary Data

364. Observation of a reduced-turbulence regime with boron powder injection in a stellarator

385. Type-I ELM mitigation by continuous lithium granule gravitational injection into the upper tungsten divertor in EAST

387. Why is El Nino warm?