Results 81 to 90 of about 11,557,211 (324)
Some Unusual Forms of Development of Equatorial Spread-F [PDF]
195-197Besides the normal development of equatorial spread-F at the base of the F-layer and later its extension at higher heights, it has been shown that the spread-F can, at times, start at the peak of the F-Iayer and then extend down during clear ...
Koparkar, P V, Chandra, H
core
Redshifting TADF Emission With a Bora‐Triptycene Lewis Acid
Bathochromic emission shifting of donor–acceptor and multi‐resonant TADF emitters is achieved by adduct formation with a thia‐bora‐triptycene Lewis acid. TADF properties are retained on adduct formation whilst delivering > 100 nm redshift of the emission.
Mathew J. Cross +4 more
wiley +1 more source
LiMn2O4${\rm LiMn}_2{\rm O}_4$ is of high interest for sustainable energy storage and conversion. Its mixed‐valence Mn3+${\rm Mn}^{3+}$/Mn4+${\text{Mn}}^{4+}$ structure drives site‐specific behavior at aqueous interfaces, featuring proton‐generating Mn4+${\text{Mn}}^{4+}$ centers and electron‐rich Mn3+${\rm Mn}^{3+}$ sites that render the surrounding ...
K. Nikolas Lausch +3 more
wiley +1 more source
Click‐to‐release (C2R) chemistry is redirected from payload liberation toward ligand‐directed covalent protein labeling through a transient dihydropyridazine methide (DHP‐methide). This concept opens the way to dual‐functional systems combining covalent target engagement with controlled effector release.
Dóra Kern +9 more
wiley +1 more source
NUMERICAL SIMULATIONS OF LARGE SCALE EQUATORIAL SPREAD F
We have performed numerical simulations of nonlinear evolution of plasma interchange instability in equatorial spread F(ESF) under different conditions. It is shown that the interchange instability resulting from one-or two-dimensional initial density perturbations can grow into plasma bubbles but cannot evolve into the plumelike structures on the west
null HUANG CHAO-SONG, null M.C.KELLEY
openaire +1 more source
Equatorial spread-F initiation: Post-sunset vortex, thermospheric winds, gravity waves
We present experimental evidence and modeling results which indicate that eastward thermospheric wind is the primary controlling factor of equatorial spread-F initiation in the post-sunset ionosphere.
Milla, Marco +4 more
core +1 more source
Atmospheric water harvesting (AWH) under arid conditions requires desiccants that load water below 30% RH and regenerate below 60°C, a performance regime traditionally limited to physisorbents. Here, we show that the inherent hydrolytic instability of M′FSIX‐25‐M coordination networks enable regeneration‐optimized chemisorbents (ROCs) with projected ...
Xiang‐Jing Kong +15 more
wiley +1 more source
Interaction of plasma drifts: A hypothesis for equatorial spread F occurrence
Studies on the generation mechanisms of post-sunset ionospheric irregularities, which constitute a threat to trans-ionospheric radio propagation, particularly at the African sector, are quite sparse.
Oyeyemi Elijah Oyedola +5 more
doaj +1 more source
Nature of Equatorial Spread-F Irregularities Derived from Spaced Fading Records at Thumba [PDF]
266-268Spaced fading records of nighttime F-region echoes over Thumba are compared on spread-F days and non-spread-F days. The fading rate is considerably low on non- spread-F days.
Chandra, H, Rastogi, R G
core
Spread-F and ionization anomaly belt
The present investigation attempts to bring out the dynamics of the F-region at magnetic equatorial and low latitudes in the American zone. Data are examined for two sets of nights, one with strong range-type spread at Huancayo another with complete ...
Rastogi, R. G. +2 more
core +1 more source

