Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/7073| DC Field | Value | Language |
|---|---|---|
| dc.contributor.authorall | Perrone, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia | en |
| dc.contributor.authorall | Mikhailov, A. V.; Pushkov Institute of Terrestrial Magnetism, Ionosphere and Radio Wave Propagation, Troitsk, Russia | en |
| dc.contributor.authorall | Korsunova, L. P.; Pushkov Institute of Terrestrial Magnetism, Ionosphere and Radio Wave Propagation, Troitsk, Russia | en |
| dc.date.accessioned | 2011-07-15T12:54:30Z | en |
| dc.date.available | 2011-07-15T12:54:30Z | en |
| dc.date.issued | 2011-06-08 | en |
| dc.identifier.uri | http://hdl.handle.net/2122/7073 | en |
| dc.description.abstract | Ionosonde observations at Rome and Gibilmanna (Sicily) for some months of 2006–2007 were analyzed in the connection with recent COSMIC NmE results. Italy was completely located in the NmE enhanced zone according to COSMIC observations for the periods in question. COSMIC‐observed NmE values in the NmE enhanced zone do not coincide with NmE scaled from ionograms in accordance with the URSI Recommendations, but the IRI model correctly describes monthly median NmE contrary to the Chu et al. (2009) conclusion. Three month averaged COSMIC NmE values turn out to be close to monthly median NmE corresponding to the blanketing frequency fbEs. A conclusion is made that sporadic E practically permanently existing during daytime hours in summer strongly contributes to NmE observed by COSMIC. Possible reasons for the occurrence of the NmE enhanced zones at middle latitudes are discussed. | en |
| dc.language.iso | English | en |
| dc.publisher.name | American Geophysical Union | en |
| dc.relation.ispartof | Journal of Geophysical Research | en |
| dc.relation.ispartofseries | /116 (2011) | en |
| dc.subject | mid-latitude ionosphere | en |
| dc.subject | sporadic E layer | en |
| dc.title | FORMOSAT-3/COSMIC E region observations and daytime foE at middle latitudes | en |
| dc.type | article | en |
| dc.description.status | Published | en |
| dc.type.QualityControl | Peer-reviewed | en |
| dc.description.pagenumber | A06307 | en |
| dc.subject.INGV | 01. Atmosphere::01.02. Ionosphere::01.02.99. General or miscellaneous | en |
| dc.subject.INGV | 01. Atmosphere::01.02. Ionosphere::01.02.02. Dynamics | en |
| dc.identifier.doi | 10.1029/2010JA016411 | en |
| dc.relation.references | Banks, P. M., and G. Kockarts (1973), Aeronomy, Academic, New York. Bilitza, D., and B. Reinisch (2008), International Reference Ionosphere 2007: Improvements and new parameters, Adv. Space Res., 42, 599–609, doi:10.1016/j.asr.2007.07.048. Chu, Y.‐H., K.‐H. Wu, and C.‐L. Su (2009), A new aspect of ionospheric E region electron density morphology, J. Geophys. Res., 114, A12314, doi:10.1029/2008JA014022. Chu, Y.‐H., K.‐H. Wu, and C.‐L. Su (2010), Reply to comment by Lei et al. on “A new aspect of ionospheric E region electron density morphology,” J. Geophys. Res., 115, A07314, doi:10.1029/2010JA015334. Hedin, A. E. (1987), MSIS‐86 thermospheric model, J. Geophys. Res., 92, 4649–4662, doi:10.1029/JA092iA05p04649. Hierl, P. M., I. Dotan, J. V. Seeley, J. M. Van Doran, R. A. Morris, and A. A. Viggiano (1997), Rate coefficients for the reactions of O+ with N2 and O2 as a function of temperature (300–1800 K), J. Chem. Phys., 106(9), 3540–3544, doi:10.1063/1.473450. Lei, J., X. Yue, and W. S. Schreiner (2010), Comment on “A new aspect of ionospheric E region electron density morphology” by Yen‐Hsyang Chu, Kong‐Hong Wu, and Ching‐Lun Su, J. Geophys. Res., 115, A07313, doi:10.1029/2009JA015234. Radio Research Laboratory (1986), URSI Manual: Manual of Ionogram Scaling, rev. ed., Minist. of Posts and Telecommun., Tokyo. Mathews, J. D. (1998), Sporadic E: Current views and recent progress, J. Atmos. Sol. Terr. Phys., 60, 413–435, doi:10.1016/S1364-6826(97) 00043-6. Nicolls, M. J., F. S. Rodrigues, G. S. Bust, and J. L. Chau (2009), Estimating E region density profiles from radio occultation measurements by IDA4D, J. Geophys. Res., 114, A10316, doi:10.1029/2009JA014399. Rao, C. S. R. (1964), Sporadic‐E and the equatorial electrojet, J. Atmos. Terr. Phys., 26, 417–427, doi:10.1016/0021-9169(64)90088-1. Rastogi, R. G., and V. L. Patel (1975), Effect of interplanetary magnetic field on ionosphere over the magnetic equator, Proc. Ind. Acad. Sci., 82A, 121–141. Rastogi, R. G., G. K. Rangarajan, and V. V. Somayajulu (1992), Complexities of counter equatorial electrojet currents, Indian J. Radio Space Phys., 21, 89–96. Robinson, B. J. (1959), Experimental investigation of the ionospheric E‐layer, Rep. Prog. Phys., 22, 241–279, doi:10.1088/0034-4885/22/1/ 308. Thomas, J. A., and E. K. Smith (1959), A survey of the present knowledge of sporadic E ionization, J. Atmos. Terr. Phys., 13, 295–314, doi:10.1016/0021-9169(59)90121-7. Whitehead, J. D. (1961), The formation of the sporadic E layer in the temperate zones, J. Atmos. Sol. Terr. Phys., 20, 49–58, doi:10.1016/0021- 9169(61)90097-6. Whitehead, J. D. (1989), Recent work on mid‐latitude and equatorial sporadic E, J. Atmos. Sol. Terr. Phys., 51, 401–424, doi:10.1016/0021-9169 (89)90122-0. Wu, D. L., C. O. Ao, G. A. Hajj, M. Torr Juarez, and A. J. Mannucci (2005), Sporadic E morphology from GPS‐CHAMP radio occultation, J. Geophys. Res., 110, A01306, doi:10.1029/2004JA010701. | en |
| dc.description.obiettivoSpecifico | 1.7. Osservazioni di alta e media atmosfera | en |
| dc.description.journalType | JCR Journal | en |
| dc.description.fulltext | restricted | en |
| dc.contributor.author | Perrone, L. | en |
| dc.contributor.author | Mikhailov, A. V. | en |
| dc.contributor.author | Korsunova, L. P. | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia | en |
| dc.contributor.department | Pushkov Institute of Terrestrial Magnetism, Ionosphere and Radio Wave Propagation, Troitsk, Russia | en |
| dc.contributor.department | Pushkov Institute of Terrestrial Magnetism, Ionosphere and Radio Wave Propagation, Troitsk, Russia | en |
| item.languageiso639-1 | en | - |
| item.cerifentitytype | Publications | - |
| item.openairetype | article | - |
| item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
| item.fulltext | With Fulltext | - |
| item.grantfulltext | restricted | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia | - |
| crisitem.author.dept | Pushkov Institute of Terrestrial Magnetism, Ionosphere and Radio Wave Propagation (IZMIRAN), Troitsk, Moscow Region 142190, Russia | - |
| crisitem.author.dept | Pushkov Institute of Terrestrial Magnetism, Ionosphere and Radio Wave Propagation (IZMIRAN), Troitsk, Moscow Region 142190, Russia | - |
| crisitem.author.orcid | 0000-0003-4335-0345 | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.classification.parent | 01. Atmosphere | - |
| crisitem.classification.parent | 01. Atmosphere | - |
| Appears in Collections: | Article published / in press | |
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| 2010JA016411.pdf | 533.56 kB | Adobe PDF |
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