Morphology and dynamics of daytime mid-latitude sporadic-E patches revealed by GPS total electron content observations in Japan
暂无分享,去创建一个
Kosuke Heki | K. Heki | Jun Maeda | J. Maeda
[1] M. Larsen,et al. Sporadic E layer observations over Arecibo using coherent and incoherent scatter radar: Assessing dynamic stability in the lower thermosphere , 2009 .
[2] Jens Wickert,et al. A global climatology of ionospheric irregularities derived from GPS radio occultation , 2008 .
[3] Jens Wickert,et al. Semidiurnal tidal signature in sporadic E occurrence rates derived from GPS radio occultation measurements at higher midlatitudes , 2009 .
[4] C. Haldoupis. Midlatitude Sporadic E. A Typical Paradigm of Atmosphere-Ionosphere Coupling , 2012 .
[5] David L. Hysell,et al. Common volume coherent and incoherent scatter radar observations of mid-latitude sporadic E-layers and QP echoes , 2004 .
[6] Takashi Tanaka. Sky-wave backscatter observations of sporadic-E over Japan , 1979 .
[7] Kosuke Heki,et al. Two‐dimensional observations of midlatitude sporadic E irregularities with a dense GPS array in Japan , 2014 .
[8] H. Maéda. Horizontal Wind Systems in the Ionospheric E Region Deduced from the Dynamo Theory of the Geomagnetic Sq Variation Part III , 1955 .
[9] T. Yokoyama,et al. Three‐dimensional simulation of the coupled Perkins and Es‐layer instabilities in the nighttime midlatitude ionosphere , 2008 .
[10] Mamoru Yamamoto,et al. Mid‐latitude E region field‐aligned irregularities observed with the MU radar , 1991 .
[11] M. Larsen,et al. Imaging coherent scatter radar, incoherent scatter radar, and optical observations of quasiperiodic structures associated with sporadic E layers , 2007 .
[12] M. Yamamoto,et al. A possible mechanism for echo striation generation of radar backscatter from midlatitude sporadic E , 2000 .
[13] D. Pancheva,et al. Terdiurnal tidelike variability in sporadic E layers , 2006 .
[14] J. Whitehead. Recent work on mid-latitude and equatorial sporadic-E , 1989 .
[15] R. Tsunoda,et al. A direction‐dependent instability of sporadic‐E layers in the nighttime midlatitude ionosphere , 2002 .
[16] M. Larsen,et al. A shear instability seeding mechanism for quasiperiodic radar echoes , 2000 .
[17] T. Maruyama. Observations of quasi‐periodic scintillations and their possible relation to the dynamics of Es plasma blobs , 1991 .
[18] M. Yamamoto,et al. Seek S310‐25: Quasi‐periodic echoes and polarization electric fields , 2000 .
[19] S. Kato. Horizontal Wind Systems in the Ionospheric E region Deduced from the Dynamo Theory of the Geomagnetic Sq Variation Part IV , 1957 .
[20] Masaru Ozeki,et al. Ionospheric holes made by ballistic missiles from North Korea detected with a Japanese dense GPS array , 2010 .
[21] Hiroyuki Hashiguchi,et al. Observation of three‐dimensional structures of quasi‐periodic echoes associated with mid‐latitude sporadic‐E layers by MU radar ultra‐multi‐channel system , 2006 .
[22] J. Yue,et al. Large winds and wind shears caused by the nonlinear interactions between gravity waves and tidal backgrounds in the mesosphere and lower thermosphere , 2014 .
[23] M. Larsen,et al. Fine structure in midlatitude sporadic E layers , 2013 .
[24] Y. Otsuka,et al. Disappearance of equatorial plasma bubble after interaction with mid‐latitude medium‐scale traveling ionospheric disturbance , 2012 .
[25] T. Maruyama. Shapes of irregularities in the sporadic E layer producing quasi-periodic scintillations , 1995 .
[26] J. Whitehead,et al. Es structure using an HF radar , 1986 .
[27] M. Yamamoto,et al. A morphological study on mid-latitude E-region field-aligned irregularities observed with the MU radar , 1992 .
[28] M. Larsen,et al. The SEEK Chemical Release Experiment: Observed neutral wind profile in a region of sporadic E , 1998 .
[29] Paul A. Bernhardt,et al. The modulation of sporadic-E layers by Kelvin–Helmholtz billows in the neutral atmosphere , 2002 .
[30] Russell B. Cosgrove,et al. Instability of the E‐F coupled nighttime midlatitude ionosphere , 2003 .
[31] S. Kato. Horizontal Wind Systems in the Ionospheric E region Deduced from the Dynamo Theory of the Geomagnetic Sq variation Part II. Rotating Earth , 1956 .
[32] Yen-Hsyang Chu,et al. Coordinated sporadic E layer observations made with Chung-Li 30 MHz radar, ionosonde and FORMOSAT-3/COSMIC satellites , 2011 .
[33] Mamoru Yamamoto,et al. Gravity wave modulation of gradient drift instabilities in mid-latitude sporadic E irregularities , 1991 .
[34] Anthony J. Mannucci,et al. Sporadic E morphology from GPS‐CHAMP radio occultation , 2005 .
[35] W. Elford. A study of winds between 80 and 100 km in medium latitudes , 1959 .
[36] M. Yamamoto,et al. Spatial structure of the E region field-aligned irregularities revealed by the MU radar , 1994 .
[37] Miguel F. Larsen,et al. Winds and shears in the mesosphere and lower thermosphere: Results from four decades of chemical release wind measurements , 2002 .
[38] L. Lomidze,et al. Double atmospheric gravity wave frequency oscillations of sporadic E formed in a horizontal shear flow , 2010 .
[39] David L. Hysell,et al. Imaging radar observations and theory of type I and type II quasi‐periodic echoes , 2002 .
[40] S. Nozawa,et al. Horizontal structure of sporadic E layer observed with a rocket‐borne magnesium ion imager , 2010 .
[41] M. Yamamoto,et al. Radar observations of field-aligned plasma irregularities in the SEEK-2 campaign , 2005 .