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1

Self-consistent modelling of the daytime electron density profile in the ionospheric F region

by A. Mikhailov, K. Schlegel
Published in Annales Geophysicae (1997)
“...A theoretical self-consistent method for the description of daytime N e (h) profiles...”

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Select result number 2
2

Unusually high frequency natural VLF radio emissions observed during daytime in Northern Finland

by Jyrki Manninen, Tauno Turunen, Natalia Kleimenova, Michael Rycroft, Liudmila Gromova, Iina Sirviö
Published in Environmental Research Letters (2016)

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3

Physical mechanism of strong negative storm effects in the daytime ionospheric F2 region observed with EISCAT

by A. Mikhailov, K. Schlegel
Published in Annales Geophysicae (1998)
“...A self-consistent method for daytime F-region modelling was applied to EISCAT observations during...”

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4

An accuracy assessment of the CALIOP/CALIPSO version 2/version 3 daytime aerosol extinction product based on a detailed multi-sensor, multi-platform case study

by M. Kacenelenbogen, M. A. Vaughan, J. Redemann, R. M. Hoff, R. R. Rogers, R. A. Ferrare, P. B. Russell, C. A. Hostetler, J. W. Hair, B. N. Holben
Published in Atmospheric Chemistry and Physics (2011)
“... in the CALIOP daytime attenuated backscatter coefficient profiles. The use of version 3 CALIOP extinction...”

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5

Observations of I 2 at a remote marine site

by M. J. Lawler, A. S. Mahajan, A. Saiz-Lopez, E. S. Saltzman
Published in Atmospheric Chemistry and Physics (2014)
“... to explain the observed daytime IO levels at this site. Iodocarbon measurements made in this region...”

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6

Anomalous variations of Nm F2 over the Argentine Islands: a statistical study

by A. V. Pavlov, N. M. Pavlova
Published in Annales Geophysicae (2009)
“... the Argentine Islands ionosonde was carried out. The variations in a maximum daytime value, R , of a ratio of a...”

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7

Primary cosmic ray electrons and albedo electrons in 1967 at energies between 12 and 1000 MEV

by Israel, Martin Henry
Published 1969
“... [.....] 100 MeV. The nighttime flux is significantly lower than the splash albedo, while the daytime flux...”

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8

Evaluation of the Snow-Ice Enhanced Weather Research and Forecasting Model

by Wiles, Jackson
Published 2019
“... 11.5-15.5 Universal Time Coordinated (UTC) for daytime and 08-12 UTC for nighttime. In the evaluation...”

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9

Model interpretation of the ionospheric F-region electron density structures observed by ground-based satellite tomography at sub-auroral and auroral latitudes in Russia in January...

by A. N. Namgaladze, O. V. Evstafiev, B. Z. Khudukon, A. A. Namgaladze
Published in Annales Geophysicae (2003)
“... with the tomography measured electron densities, whereas UAM has the best agreement with the daytime tomography...”

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10

Different strategies to retrieve aerosol properties at night-time with the GRASP algorithm

by J. A. Benavent-Oltra, R. Román, J. A. Casquero-Vera, D. Pérez-Ramírez, H. Lyamani, P. Ortiz-Amezcua, A. E. Bedoya-Velásquez, G. de Arruda Moreira, Á. Barreto, A. Lopatin, D. Fuertes, M. Herrera, B. Torres, O. Dubovik, J. L. Guerrero-Rascado, P. Goloub, F. J. Olmo-Reyes, L. Alados-Arboledas
Published in Atmospheric Chemistry and Physics (2019)
“... campaign. For daytime aerosol retrievals, we combined the measurements of the ground-based lidar from...”

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Select result number 11
11

High temporal resolution Br 2 , BrCl and BrO observations in coastal Antarctica

by R. von Glasow, D. J. Tanner, L. G. Huey, N. Brough, Z. Buys, A. E. Jones
Published in Atmospheric Chemistry and Physics (2013)
“...). We find indications for an artefact in daytime BrCl measurements arising from conversion of HOBr...”

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12

What Happens to Nighttime Power Plant Emissions

by Thompson, Chelia
Published 2019
“... 11.5-15.5 Universal Time Coordinated (UTC) for daytime and 08-12 UTC for nighttime. In the evaluation...”

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13

The representation of the trade winds in ECMWF forecasts and reanalyses during EUREC 4 A

by A. C. M. Savazzi, L. Nuijens, I. Sandu, G. George, P. Bechtold
Published in Atmospheric Chemistry and Physics (2022)
“... diurnal cycle that is too strong, leading to a weak wind speed bias everywhere up to 5 km during daytime...”

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14

Trends in Occurrence of Polar Cap SuperDARN Echoes and Electron Density Variations in the Ionosphere

by Ullrich, Syd
Published 2021
“... scatter radar within RKNs field of view. Reasonable agreement between the instruments is shown for daytime...”

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15

Morphology of the spectral resonance structure of the electromagnetic background noise in the range of 0.1–4 Hz at L = 5.2

by A. G. Yahnin, N. V. Semenova, A. A. Ostapenko, J. Kangas, J. Manninen, T. Turunen
Published in Annales Geophysicae (2003)
“... that the occurrence rate of SRS is higher in the nighttime than in the daytime. The occurrence rate is higher...”

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16

ULF geomagnetic pulsations at different latitudes in Antarctica

by P. Francia, M. De Lauretis, M. Vellante, U. Villante, A. Piancatelli
Published in Annales Geophysicae (2009)
“... to the cusp and closed field lines in the daytime, the ULF power is characterized by a maximum around noon...”

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17

Climatological features of electron density in the polar ionosphere from long-term observations of EISCAT/ESR radar

by H. T. Cai, S. Y. Ma, Y. Fan, Y. C. Liu, K. Schlegel
Published in Annales Geophysicae (2007)
“... is evident during the solar maximum at EISCAT, but it dies out at the latitude of the ESR; (2) The daytime...”

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18

Simultaneous observations of large-scale traveling ionospheric disturbances on the nightside and dayside middle latitude

by H. T. Cai, F. Yin, S. Y. Ma, J. S. Xu, Y. W. Liu
Published in Annales Geophysicae (2012)
“... are separated by hundreds of kilometers longitudinally. Periods of the daytime and nighttime ionospheric...”

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19

The MIPAS HOCl climatology

by T. von Clarmann, B. Funke, N. Glatthor, S. Kellmann, M. Kiefer, O. Kirner, B.-M. Sinnhuber, G. P. Stiller
Published in Atmospheric Chemistry and Physics (2012)
“... at higher altitudes than during daytime. Particularly low values (below 80 ppt) during daytime are found...”

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20

Contrasting atmospheric boundary layer chemistry of methylhydroperoxide (CH 3 OOH) and hydrogen peroxide (H 2 O 2 ) above polar snow

by D. K. Friel, J. F. Burkhart, S. J. Sjostedt, M. A. Hutterli, G. Chen, M. M. Frey, R. C. Bales
Published 2009
“..., respectively. In early spring, MHP dominated the ROOH budget and showed night time maxima and daytime minima...”

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