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  • 1
    Call number: 21/STR 96/13
    In: Scientific Technical Report STR
    Type of Medium: GFZ publications
    Pages: 24 S.
    Series Statement: Scientific Technical Report STR 96/13
    Classification:
    Photogrammetry, Remote Sensing
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
    Publication Date: 2021-03-29
    Description: We sketch the eventful life of Willy Stoffregen and summarise his engineering and scientific achievements.
    Keywords: Willy Stoffregen; pioneer; advanced ionospheric; auroral research ; 551
    Language: English
    Type: article , publishedVersion
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  • 3
    Publication Date: 2020-02-12
    Description: The International Geomagnetic Reference Field (IGRF) is a very frequently used model of the Earth’s main magnetic field by both the science community and the industry. This model is updated every five years. We present here the second generation of the GRIMM magnetic field model that was derived to contribute to the IGRF-11. The model has been developed from a newly, reprocessed CHAMP satellite data set covering nearly 10 years. It has a temporal and spatial resolution significantly improved compared to previous models.
    Language: English
    Type: info:eu-repo/semantics/bookPart
    Format: application/pdf
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  • 4
    Publication Date: 2020-02-12
    Description: In this study we investigated conditions for loss of GPS signals observed by the Swarm satellites during a 2 year period, from December 2013 to November 2015. Our result shows that the Swarm satellites encountered most of the total loss of GPS signal at the ionization anomaly crests, between ±5° and ±20° magnetic latitude, forming two bands along the magnetic equator, and these low-latitude events mainly appear around postsunset hours from 19:00 to 22:00 local time. By further checking the in situ electron density measurements of Swarm, we found that practically, all the total loss of GPS signal events at low latitudes are related to equatorial plasma irregularities (EPIs) that show absolute density depletions larger than 10 × 1011 m−3; then, the Swarm satellites encountered for up to 95% loss of GPS signal for at least one channel and up to 45% tracked less than four GPS satellites (making precise orbit determination impossible). For those EPIs with density depletions less than 10 × 1011 m−3, the chance of tracked GPS signals less than four reduces to only 1.0%. Swarm also observed total loss of all GPS signal at high latitudes, mainly around local noon, and these events are related to large spatial density gradients due to polar patches or increased geomagnetic/auroral activities. We further found that the loss of GPS signals were less frequent after appropriate settings of the Swarm GPS receivers had been updated. However, the more recent period of the mission, e.g., after the GPS receiver settings have been updated, also coincides with less severe electron density depletions due to the declining solar cycle, making GPS loss events less likely. We conclude that both lower electron density gradients and appropriate GPS receiver settings reduce the probability for Swarm satellites loss of GPS signals.
    Language: English
    Type: info:eu-repo/semantics/article
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  • 5
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    In:  Journal of Geophysical Research: Space Physics
    Publication Date: 2020-12-14
    Description: A new empirical model of field‐aligned currents in the Earth's ionosphere has been developed. This model is derived using magnetometer data from the CHAallenging Minisatellite Payload, Ø rsted, and Swarm satellite missions, which has created a database that spans more than 15 years. These data have been associated with solar wind conditions using the Advanced Composition Explorer satellite, as well as the urn:x-wiley:jgra:media:jgra55433:jgra55433-math-0001, urn:x-wiley:jgra:media:jgra55433:jgra55433-math-0002, urn:x-wiley:jgra:media:jgra55433:jgra55433-math-0003, and urn:x-wiley:jgra:media:jgra55433:jgra55433-math-0004 solar indices. With the wealth of data and associated driving conditions, this model has been developed to reproduce field‐aligned current maps of the ionosphere based on solar wind electric field, interplanetary magnetic field clock angle, dipole tilt angle, solar index, and geographic hemisphere. This model was constructed using a series of spherical cap harmonic analysis fits based on small selections of the overall database. The coefficients of these fits were then used to develop a model that would reproduce these coefficients based on the previously described driving conditions. One of the most notable improvements demonstrated by this model is the ability to show distinct current regions in the ionosphere, particularly with respect to Region 0 currents during northward urn:x-wiley:jgra:media:jgra55433:jgra55433-math-0005 and highly positive or negative urn:x-wiley:jgra:media:jgra55433:jgra55433-math-0006.
    Language: English
    Type: info:eu-repo/semantics/article
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  • 6
    Publication Date: 2021-02-28
    Description: The GRACE (Gravity Recovery and Climate Experiment) satellites, which comprises two spacecraft, GRACE-A and GRACE-B, were launched on 17 March 2002 into a near-circular, polar (inclination = 89◦ ) orbit with an initial altitude of about 490 km. The two satellites follow each other at a distance of about 200 km. The primary objective of the GRACE mission is to provide global high-resolution models of the Earth’s gravity field. The instruments supporting our study are the K-Band Ranging System (KBR), and the GPS Space Receiver (GPS). The K-Band Ranging System (KBR) system is the key science instrument of GRACE which measures the dual one-way range change between both satellites with a precision of about 1 μm per second. From the KBR1B data we can get the change of Total Electron Content (TEC). In addition the GPS Navigation Data (GNV1B) can provide us the position of the two satellites. From these data we can derive the average electron density between the two satellites. The data are stored as daily ASCII files using the file naming convention 'KBRNE_YYYY_MM_DD.dat'. Headers in each data file contain a short name for each column. A more detailed description is provided in the readme file.
    Language: English
    Type: info:eu-repo/semantics/workingPaper
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  • 7
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    In:  Magnetospheres in the Solar System | Geophysical Monograph Series
    Publication Date: 2021-05-12
    Description: Field‐aligned currents play a major role in magnetized plasmas. They are the main agents for coupling the dynamics between magnetosphere and ionosphere. Perturbations of magnetic field distribution, plasma pressure or flow on one end are communicated by field‐aligned currents along the whole flux tube. Furthermore, they transport energy, practically lossless, from dynamo regions in the magnetosphere into the upper atmosphere. The knowledge of field‐aligned current distribution is therefore of great interest for understanding the magnetosphere‐ionosphere system. In this chapter we describe the expressions that illustrate the relationship between plasma motion in the magnetosphere and electric currents flowing along the background magnetic field. These currents can only be sensed above the ionospheric E‐layer, e.g. by low‐Earth orbiting satellites. However, to obtain reliable current density estimates is quite challenging. In a climatological sense, field‐aligned currents appear along two concentric rings in the high‐latitude ionosphere with opposite flow directions. Details of these patterns are controlled by the orientation of the interplanetary magnetic field. The transverse scale sizes determine important characteristics of field‐aligned currents.
    Language: English
    Type: info:eu-repo/semantics/bookPart
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  • 8
    Publication Date: 2021-05-12
    Description: ESA’s Swarm constellation mission consisting of three identical satellites, successfully launched on 22 November 2013, provides the excellent opportunity of reliable electric current density estimates in the ionosphere based on multi-satellite magnetic field measurements. The final constellation with Swarm A/C orbiting the Earth at about 470 km (flying side-by-side) and Swarm B at about 520 km altitude was achieved on 17 April 2014. Swarm satellites need a period of about 130 days to cover all local times; therefore the coverage of all local times and local seasons can be achieved in 5 years from the final constellation when the dual-satellite current density estimations have been started. We present the climatology of field-aligned currents (FACs) at polar cap, cusp and auroral regions, radial, interhemispheric (IHFACs) and F region dynamo currents at mid-latitude and equatorial regions, using the single and dual satellite approaches for the current density estimations. Also, the higher-flying Swarm B satellite provides from time to time well-matched observations with the 50 km lower Swarm A/C pair that gives the possibility for zonal current estimates by using Ampère’s ring integral for determining the mean current density passing through the encircled area.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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  • 9
    Publication Date: 2020-02-12
    Description: The atmospheric lunar tide is one known source of ionospheric variability. The subject received renewed attention as recent studies found a link between stratospheric sudden warmings and amplified lunar tidal perturbations in the equatorial ionosphere. There is increasing evidence from ground observations that the lunar tidal influence on the ionosphere depends on longitude. We use magnetic field measurements from the CHAMP satellite during July 2000 to September 2010 and from the two Swarm satellites during November 2013 to February 2017 to determine, for the first time, the complete seasonal-longitudinal climatology of the semidiurnal lunar tidal variation in the equatorial electrojet intensity. Significant longitudinal variability is found in the amplitude of the lunar tidal variation, while the longitudinal variability in the phase is small. The amplitude peaks in the Peruvian sector (∼285°E) during the Northern Hemisphere winter and equinoxes, and in the Brazilian sector (∼325°E) during the Northern Hemisphere summer. There are also local amplitude maxima at ∼55°E and ∼120°E. The longitudinal variation is partly due to the modulation of ionospheric conductivities by the inhomogeneous geomagnetic field. Another possible cause of the longitudinal variability is neutral wind forcing by nonmigrating lunar tides. A tidal spectrum analysis of the semidiurnal lunar tidal variation in the equatorial electrojet reveals the dominance of the westward propagating mode with zonal wave number 2 (SW2), with secondary contributions by westward propagating modes with zonal wave numbers 3 (SW3) and 4 (SW4). Eastward propagating waves are largely absent from the tidal spectrum. Further study will be required for the relative importance of ionospheric conductivities and nonmigrating lunar tides.
    Language: English
    Type: info:eu-repo/semantics/article
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  • 10
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    Deutsches GeoForschungsZentrum
    Publication Date: 2020-02-12
    Language: English
    Type: info:eu-repo/semantics/report
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