Channel modeling for reflective phased array type RISs in mmWave networks

2021 ◽  
Author(s):  
Joonas Kokkoniemi ◽  
Markku Juntti
2021 ◽  
Author(s):  
Shin-ich Sobue ◽  
Takeo Tadono ◽  
Satoko Miura ◽  
Akiko Noda ◽  
Takeshi Motooka ◽  
...  

<p>Japan Aerospace Exploration Agency (JAXA) launched its first L-band SAR mission - Japanese Earth Resources Satellite (JERS-1) in 1992. Though the design life of JERS-1 was 2 years, the satellite had obtained observational data for more than 6 years and ended the mission in 1998. Following to JERS-1, Advanced Land Observing Satellite (ALOS) was launched in 2006. ALOS was equipped with three sensors: the Phased Array type L-band SAR (PALSAR), the Panchromatic Remote-sensing Instrument for Stereo Mapping (PRISM), and the Advanced Visible and Near Infrared Radiometer type 2 (AVNIR-2). ALOS's observation data has been used in various areas including disaster mitigation through observing regions damaged by earthquakes, tsunami, or typhoons, as well as carrying out forest monitoring, natural environment maintenance, agriculture, and compiling a 1/25,000 topographical map. When the Great East Japan Earthquake hit Japan in 2011, ALOS took some 400 images over disaster-stricken areas to provide information to all parties concerned.</p><p>Technologies acquired from the ALOS are succeeded to the second Advanced Land Observing Satellite “ALOS-2.”, which was successfully launched on 24th May 2014. The mission sensor of ALOS-2 is the Phased Array type L-band Synthetic Aperture Radar-2 called PALSAR-2 which is the state-of-the-art L-band SAR system. Until now after the successful completion of initial checkout after launching, ALOS-2 has been contributed to a lot of emergency observations for natural disasters, not only in Japan but also in the world. Furthermore, based on the Basic Observation Scenario (BOS) of ALOS-2, 10m global map data and other mode data are routinely collected and archived. This paper describes the results of ALOS-2 operation in nominal operation phase and outline of future ALOS series missions, especially ALOS-4 launched JFY2022.</p>


1984 ◽  
Vol 87 (793) ◽  
pp. 1341-1346
Author(s):  
Tadao MORI ◽  
Hideo KASHIWAYA ◽  
Ichiro KOMURA ◽  
Satoshi NAGAI ◽  
Kuniharu UCHIDA

1984 ◽  
Vol 100 (3) ◽  
pp. 536 ◽  
Author(s):  
Keith D. Paulsen ◽  
John W. Strohbehn ◽  
Daniel R. Lynch

1965 ◽  
Vol 53 (10) ◽  
pp. 1666-1667 ◽  
Author(s):  
A. Korpel
Keyword(s):  

2004 ◽  
Vol 82 (3) ◽  
pp. 915-931 ◽  
Author(s):  
Hiroyuki HASHIGUCHI ◽  
Shoichiro FUKAO ◽  
Yuki MORITANI ◽  
Toshio WAKAYAMA ◽  
Shinichiro WATANABE

2016 ◽  
Vol 63 (237) ◽  
pp. 148-163 ◽  
Author(s):  
VIBHOR AGARWAL ◽  
TOBIAS BOLCH ◽  
TAJDARUL H. SYED ◽  
TINO PIECZONKA ◽  
TAZIO STROZZI ◽  
...  

ABSTRACTHere, we present a comprehensive assessment of Siachen Glacier (East Karakoram), in terms of its area and elevation change, velocity variations and mass budget, utilizing different satellite datasets including Landsat, Hexagon, Cartosat-I, Shuttle Radar Topography Mission, Envisat Advanced Synthetic Aperture Radar and Japanese Advanced Land Observing Satellite Phased Array-type L-band SAR. The total areal extent of Siachen Glacier did not change significantly between 1980 and 2014; however the exposed-ice area decreased during that period. The terminus of the glacier has experienced substantial downwasting (on average 30 m) over the period of 1999–2007, followed by a retreat of the transition between exposed and debris-covered ice by a distance of 1.3 km during the short span 2007–14. The spatial patterns of the elevation difference and velocity are heterogeneous over the large areal extent of Siachen Glacier. The average velocity of the entire glacier, as computed between 11 December 2008 and 26 January 2009, was 12.3 ± 0.4 cm d−1, while those estimated separately for the accumulation and ablation regions were 9.7 ± 0.4 cm d−1 and 20.4 ± 0.4 cm d−1, respectively. The mass budget of Siachen Glacier is estimated to be –0.03 ± 0.21 m w.e. a−1 for the period of 1999–2007.


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