Paper Session III-B - The Photon Satellite: A Demonstration of Satellite Laser Tracking and Communications

An alliance of Florida universities and companies are proposing to construct a small satellite to demonstrate the feasibility of laser communications for satellite to groundairborne receivers and ground-airborne to satellite receivers. The possibility of using high-data-rate optical transmitters for satellite communications has generated a renew interest in laser communication systems for ground-airborne-to-space and space-toground- airborne data links. Here we describe a ground to satellite experiment to demonstrate the requirements of pointing accuracy and tracking for reliable communications and a novel technique to track a satellite with laser beam

Importance of capturing heliospheric variability for studies of thermospheric vertical winds

Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/95431/1/jgra21925.pd

Small‐scale structure of the midlatitude storm enhanced density plume during the 17 March 2015 St. Patrick’s Day storm

Kilometer‐scale density irregularities in the ionosphere can cause ionospheric scintillation—a phenomenon that degrades space‐based navigation and communication signals. During strong geomagnetic storms, the midlatitude ionosphere is primed to produce these ∼1–10 km small‐scale irregularities along the steep gradients between midlatitude storm enhanced density (SED) plumes and the adjacent low‐density trough. The length scales of irregularities on the order of 1–10 km are determined from a combination of spatial, temporal, and frequency analyses using single‐station ground‐based Global Positioning System total electron content (TEC) combined with radar plasma velocity measurements. Kilometer‐scale irregularities are detected along the boundaries of the SED plume and depleted density trough during the 17 March 2015 geomagnetic storm, but not equatorward of the plume or within the plume itself. Analysis using the fast Fourier transform of high‐pass filtered slant TEC suggests that the kilometer‐scale irregularities formed near the poleward gradients of SED plumes can have similar intensity and length scales to those typically found in the aurora but are shown to be distinct phenomena in spacecraft electron precipitation measurements.Key PointsKilometer‐scale density irregularities measured in single‐station GPS TEC data from the 17 March 2015 storm enhanced density plume systemLocation, intensity, and length scales are estimated from spatial, temporal, and frequency analyses of multiple instrument dataFormation regions for small‐scale irregularities with length scales of 3‐10 km are identified for plasma velocities of 500–1200 m s−1Peer Reviewedhttps://deepblue.lib.umich.edu/bitstream/2027.42/136745/1/jgra53295_am.pdfhttps://deepblue.lib.umich.edu/bitstream/2027.42/136745/2/jgra53295.pdfhttps://deepblue.lib.umich.edu/bitstream/2027.42/136745/3/jgra53295-sup-0001-supplementary.pd

Strong postmidnight equatorial ionospheric anomaly observations during magnetically quiet periods

Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/94882/1/jgra20156.pd

Global Magnetosphere Response to Solar Wind Dynamic Pressure Pulses During Northward IMF Using the Heliophysics System Observatory

We analyzed the magnetospheric global response to dynamic pressure pulses (DPPs) using the Heliophysics System Observatory (HSO) and ground magnetometers. During northward Interplanetary Magnetic Field (IMF) Bz conditions, the magnetosphere acts as a closed “cavity” and reacts to solar wind DPPs more simply than during southward IMF. In this study we use solar wind data collected by ACE and WIND together with magnetic field observations of Geotail, Cluster, Time History of Events and Macroscale Interactions during Substorms (THEMIS), Magnetospheric Multiscale Mission (MMS), Van Allen Probes, GOES missions, and ground magnetometer arrays to observe the magnetosphere (dayside, nightside, inner magnetosphere, magnetotail, magnetosheath, etc.) and ionosphere response simultaneously in several local time sectors and regions. A total of 37 events were selected during the period between February 2007 to December 2017. We examine the global response of each event and identify systematic behavior of the magnetosphere due to DPPs' compression, such as MHD wave propagation, sudden impulses, and Ultra Low Frequency waves (ULF) in the Pc5 range. Our results confirm statistical studies with a more limited coverage that have been performed at different sectors and/or regions of the magnetosphere. We present observations of the different signatures generated in different regions that propagate through the magnetosphere. The signature of the tailward traveling DPP is observed to move at the same solar wind speed, and in superposition of other known magnetospheric perturbations. It is observed that the DPP also generates or increases the amplitude of Pc4‐5 waves observed in the inner magnetosphere, while similar waves are observed on the ground.NSF, GEO, Division of Atmospheric and Geospace Sciences. Grant Numbers: 1654044, 1450512MINEDUC, Comisión Nacional de Investigación Científica y Tecnológica. Grant Number: CONICYT PAI/INDUSTRIA 79090016Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/166313/1/2020JA028587.pdfDescription of 2020JA028587.pdf : Main ArticleSEL

On the causes of plasmaspheric rotation variability: IMAGE EUV observations

Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/95534/1/jgra20000.pd

The Effect of F‐Layer Zonal Neutral Wind on the Monthly and Longitudinal Variability of Equatorial Ionosphere Irregularity and Drift Velocity

The effect of eastward zonal wind speed (EZWS) on vertical drift velocity (E × Bdrift) that mainly controls the equatorial ionospheric irregularities has been explained theoretically and through numerical models. However, its effect on the seasonal and longitudinal variations of E × B and the accompanying irregularities has not yet been investigated experimentally due to lack of F‐layer wind speed measurements. Observations of EZWS from GOCE and ion density and E × B from C/NOFS satellites for years 2011 and 2012 during quite times are used in this study. Monthly and longitudinal variations of the irregularity occurrence, E × B, and EZWS show similar patterns. We find that at most 50.85% of longitudinal variations of E × B can be explained by the longitudinal variability of EZWS only. When the EZWS exceeds 150 m/s, the longitudinal variation of EZWS, geomagnetic field strength, and Pedersen conductivity explain 56.40–69.20% of the longitudinal variation of E × B. In Atlantic, Africa, and Indian sectors, from 42.63% to 79.80% of the monthly variations of the E × B can be explained by the monthly variations of EZWS only. It is found also that EZWS and E × B may be linearly correlated during fall equinox and December solstice. The peak occurrence of irregularity in the Atlantic sector during November and December is due to the combined effect of large wind speed, solar terminator‐geomagnetic field alignment, and small geomagnetic field strength and Pedersen conductivity. Moreover, during June solstices, small EZWS corresponds to vertically downward E × B, which suggests that other factors dominate the E × B drift rather than the EZWS during these periods.Key PointsZonal neutral wind controls more the seasonal variations of E × B drift than the longitudinal variations of E × B driftAt most 50.85% of the longitudinal variations of E × B drift are accounted for by the eastward zonal neutral wind speed onlyZonal neutral wind speed and E × B drift may be linearly correlated during fall equinox and December solsticePeer Reviewedhttps://deepblue.lib.umich.edu/bitstream/2027.42/155994/1/jgra55709.pdfhttps://deepblue.lib.umich.edu/bitstream/2027.42/155994/2/jgra55709_am.pd

Quantifying the azimuthal plasmaspheric density structure and dynamics inferred from IMAGE EUV

Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/95221/1/jgra22185.pd

GPS TEC observations of dynamics of the mid‐latitude trough during substorms

Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/95166/1/grl28288.pd

Storm Time Global Observations of Largeâ Scale TIDs From Groundâ Based and In Situ Satellite Measurements

This paper discusses the ionosphere’s response to the largest storm of solar cycle 24 during 16â 18 March 2015. We have used the Global Navigation Satellite Systems (GNSS) total electron content data to study largeâ scale traveling ionospheric disturbances (TIDs) over the American, African, and Asian regions. Equatorward largeâ scale TIDs propagated and crossed the equator to the other side of the hemisphere especially over the American and Asian sectors. Poleward TIDs with velocities in the range â 400â 700 m/s have been observed during local daytime over the American and African sectors with origin from around the geomagnetic equator. Our investigation over the American sector shows that poleward TIDs may have been launched by increased Lorentz coupling as a result of penetrating electric field during the southward turning of the interplanetary magnetic field, Bz. We have observed increase in SWARM satellite electron density (Ne) at the same time when equatorward largeâ scale TIDs are visible over the Europeanâ African sector. The altitude Ne profiles from ionosonde observations show a possible link that stormâ induced TIDs may have influenced the plasma distribution in the topside ionosphere at SWARM satellite altitude.Key PointsIncreased SWARM in situ electron density toward high latitudes in presence of equatorward largeâ scale TIDsEvidence of equatorward TIDs in influencing altitudinal plasma distribution to the topside ionospherePossibility of poleward TIDs launched from the geomagnetic equatorial region with comparable velocity values in both hemispheresPeer Reviewedhttps://deepblue.lib.umich.edu/bitstream/2027.42/142539/1/jgra53978_am.pdfhttps://deepblue.lib.umich.edu/bitstream/2027.42/142539/2/jgra53978.pd