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2 results on '"Sarris, T. (Theodoros)"'

1. Plasma-neutral interactions in the lower thermosphere-ionosphere:the need for in situ measurements to address focused questions

Author

Sarris, T. (Theodoros), Palmroth, M. (Minna), Aikio, A. (Anita), Buchert, S. C. (Stephan Christoph), Clemmons, J. (James), Clilverd, M. (Mark), Dandouras, I. (Iannis), Doornbos, E. (Eelco), Goodwin, L. V. (Lindsay Victoria), Grandin, M. (Maxime), Heelis, R. (Roderick), Ivchenko, N. (Nickolay), Moretto-Jørgensen, T. (Therese), Kervalishvili, G. (Guram), Knudsen, D. (David), Liu, H.-L. (Han-Li), Lu, G. (Gang), Malaspina, D. M. (David M.), Marghitu, O. (Octav), Maute, A. (Astrid), Miloch, W. J. (Wojciech J.), Olsen, N. (Nils), Pfaff, R. (Robert), Stolle, C. (Claudia), Talaat, E. (Elsayed), Thayer, J. (Jeffrey), Tourgaidis, S. (Stelios), Verronen, P. T. (Pekka T.), Yamauchi, M. (Masatoshi), Sarris, T. (Theodoros), Palmroth, M. (Minna), Aikio, A. (Anita), Buchert, S. C. (Stephan Christoph), Clemmons, J. (James), Clilverd, M. (Mark), Dandouras, I. (Iannis), Doornbos, E. (Eelco), Goodwin, L. V. (Lindsay Victoria), Grandin, M. (Maxime), Heelis, R. (Roderick), Ivchenko, N. (Nickolay), Moretto-Jørgensen, T. (Therese), Kervalishvili, G. (Guram), Knudsen, D. (David), Liu, H.-L. (Han-Li), Lu, G. (Gang), Malaspina, D. M. (David M.), Marghitu, O. (Octav), Maute, A. (Astrid), Miloch, W. J. (Wojciech J.), Olsen, N. (Nils), Pfaff, R. (Robert), Stolle, C. (Claudia), Talaat, E. (Elsayed), Thayer, J. (Jeffrey), Tourgaidis, S. (Stelios), Verronen, P. T. (Pekka T.), and Yamauchi, M. (Masatoshi)

Abstract

The lower thermosphere-ionosphere (LTI) is a key transition region between Earth’s atmosphere and space. Interactions between ions and neutrals maximize within the LTI and in particular at altitudes from 100 to 200 km, which is the least visited region of the near-Earth environment. The lack of in situ co-temporal and co-spatial measurements of all relevant parameters and their elusiveness to most remote-sensing methods means that the complex interactions between its neutral and charged constituents remain poorly characterized to this date. This lack of measurements, together with the ambiguity in the quantification of key processes in the 100–200 km altitude range affect current modeling efforts to expand atmospheric models upward to include the LTI and limit current space weather prediction capabilities. We present focused questions in the LTI that are related to the complex interactions between its neutral and charged constituents. These questions concern core physical processes that govern the energetics, dynamics, and chemistry of the LTI and need to be addressed as fundamental and long-standing questions in this critically unexplored boundary region. We also outline the range of in situ measurements that are needed to unambiguously quantify key LTI processes within this region, and present elements of an in situ concept based on past proposed mission concepts.

Published
2023

2. Lower-thermosphere–ionosphere (LTI) quantities:current status of measuring techniques and models

Author

Palmroth, M. (Minna), Grandin, M. (Maxime), Sarris, T. (Theodoros), Doornbos, E. (Eelco), Tourgaidis, S. (Stelios), Aikio, A. (Anita), Buchert, S. (Stephan), Clilverd, M. A. (Mark A.), Dandouras, I. (Iannis), Heelis, R. (Roderick), Hoffmann, A. (Alex), Ivchenko, N. (Nickolay), Kervalishvili, G. (Guram), Knudsen, D. J. (David J.), Kotova, A. (Anna), Liu, H.-L. (Han-Li), Malaspina, D. M. (David M.), March, G. (Gunther), Marchaudon, A. (Aurelie), Marghitu, O. (Octav), Matsuo, T. (Tomoko), Miloch, W. J. (Wojciech J.), Moretto-Jorgensen, T. (Therese), Mpaloukidis, D. (Dimitris), Olsen, N. (Nils), Papadakis, K. (Konstantinos), Pfaff, R. (Robert), Pirnaris, P. (Panagiotis), Siemes, C. (Christian), Stolle, C. (Claudia), Suni, J. (Jonas), van den IJssel, J. (Jose), Verronen, P. T. (Pekka T.), Visser, P. (Pieter), and Yamauchi, M. (Masatoshi)

Abstract

The lower-thermosphere–ionosphere (LTI) system consists of the upper atmosphere and the lower part of the ionosphere and as such comprises a complex system coupled to both the atmosphere below and space above. The atmospheric part of the LTI is dominated by laws of continuum fluid dynamics and chemistry, while the ionosphere is a plasma system controlled by electromagnetic forces driven by the magnetosphere, the solar wind, as well as the wind dynamo. The LTI is hence a domain controlled by many different physical processes. However, systematic in situ measurements within this region are severely lacking, although the LTI is located only 80 to 200 km above the surface of our planet. This paper reviews the current state of the art in measuring the LTI, either in situ or by several different remote-sensing methods. We begin by outlining the open questions within the LTI requiring high-quality in situ measurements, before reviewing directly observable parameters and their most important derivatives. The motivation for this review has arisen from the recent retention of the Daedalus mission as one among three competing mission candidates within the European Space Agency (ESA) Earth Explorer 10 Programme. However, this paper intends to cover the LTI parameters such that it can be used as a background scientific reference for any mission targeting in situ observations of the LTI.

Published
2021

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