Ice studies: Visit to the Radio Physics Laboratory of the Arctic and Antarctic Research Institute in Leningrad

Eos ◽  
1979 ◽  
Vol 60 (10) ◽  
pp. 151 ◽  
Author(s):  
Charles R. Bentley
2020 ◽  
Author(s):  
Peter Stauning

Abstract. In the publication Troshichev et al. (2006) on the Polar Cap (PC) indices, PCN (North) and PCS (South), an error was made by using components of the Interplanetary Magnetic Field (IMF) in their Geocentric Solar Ecliptic (GSE) representation instead of the prescribed Geocentric Solar Magnetosphere (GSM) representation for calculations of index scaling parameters in the version AARI_1998-2001 (named AARI#3) issued from the Arctic and Antarctic Research Institute (AARI) in St Petersburg, Russia. The mistake has caused a trail of incorrect relations and wrong conclusions extending since 2006 up to now (2020). The authors of the publication commented here, Troshichev, Podorozhkina, Janzhura (2011): Invariability of relationship between the polar cap magnetic activity and geoeffective interplanetary electric field, Ann. Geophys., 29, 1479-1489, state that they have used scaling parameters of the (invalid) AARI#3 PC index version in their work but have substituted parameters from the more recent AARI_1995-2005 (AARI#4) version instead. The mingling of PC index versions have resulted in erroneous illustrations in their Figs. 1, 2, 3, 6, 7, and 8 and the issuing of non-substantiated statements.


2015 ◽  
Vol 55 (4) ◽  
pp. 127 ◽  
Author(s):  
G. V. Alekseev ◽  
D. Yu. Bolshiyanov ◽  
V. F. Radionov ◽  
S. V. Frolov

Author(s):  
Nabil Panchi ◽  
Ekaterina Kim ◽  
Sheng Xu

Abstract This study investigates whether the vessels remain within their operational limitations in ice using the risk index calculated based on the Polar Operational Limitations Assessment Risk Indexing System (POLARIS) — an acceptable methodology for the assessment of operational limitations in ice infested waters, referenced in the Polar Code of the International Maritime Organization (IMO). The speeds and positions of the vessels in the Kara Sea region were analyzed from January through April for 2017–2019 using the navigational data provided by the Northern Sea Route Administration. For each vessel, except for the icebreakers, the risk index based on POLARIS was calculated using the open-access ice information that was provided by the Arctic and Antarctic Research Institute in Russia. The variation of risk index was analyzed with respect to various parameters such as the ice-class of the vessel, the reported operating speed of the vessel, and the built year of the vessel. Furthermore, we explored the limitations of the risk assessment system as well as the limitations of the available ice information and its implications on the risk assessment system. This paper reports preliminary results from the analysis.


2019 ◽  
Vol 98 (1) ◽  
pp. 17-21 ◽  
Author(s):  
Dmitry Yu. Vlasov ◽  
Sh. B. Teshebaev ◽  
M. S. Zelenskaya ◽  
I. Yu. Kirtsideli ◽  
Yu. V. Ryabusheva

The article presents the results of mycological analysis of samples taken from open surfaces in residential and working areas of the Arctic and Antarctic Research Institute (AARI) station on the Bolshevik island of the Northern Land archipelago. 114 samples were studied during the expedition work from 2014 to 2016. In total, 47 species of micromycetes were detected in the course of the research. Most of the species (89%) were identified as Ascomycetes. Mucor group of fungi was composed 11% out of all the identified species. The genus Penicillium was the richest in species diversity (16 species). On the surface of materials in places of the increased moisture, there was an open growth of colonies of the Penicillium species. P. expansum was the dominant one, being noted during all the years of observations with the occurrence of about 60%. Among the frequently occurring species, there were P. brevicompactum, P. herqueri, P. purpurogenum and P. waksmanii, which were also noted during all the years of observation (the total occurrence exceeded 15%, although in some years it was much higher). Dark-colored fungus Cladosporium cladosporioides was also dominated species, which in some cases formed black mold on the surface of the materials. Among the potential pathogens, 41 species were registered. A comparison of the data obtained over the years indicates in 2016 the largest number of microfungi to be detected in the indoor environment of AARI station (35 species), whereas in 2014 and 2015 only 29 species of fungi were identified. The similarity of the identified groups of fungi over the years turned out to be quite high. Approximately 36% of microfungi (17 species) were observed annually, although their occurrence over the years varied significantly. Locally accumulation of micromycetes was noted in the indoor environment: household rooms, storage places, workrooms. In these cases, the microfungi colonized the colorful coating, synthetic materials, plywood. The formation of mycobiota in the studied areas is due to anthropogenic invasion of microfungi.


2017 ◽  
Author(s):  
Juha Karvonen

Abstract. Here we present a method for estimating the land-fast ice (LFI) extent from SENTINEL-1 SAR mosaics over an Arctic study area over Kara and Barents Seas. The method is based on temporal cross-correlation between adjacent day SAR mosaics. The results are compared to the LFI of the Russian Arctic-Antarctic Research Institute (AARI) ice charts. A LFI time series covering the time period from October 2015 to the end of August 2017 computed using the presented methodology is provided on our ftp server. The time series will be extended twice annually.


Polar Record ◽  
2019 ◽  
Vol 55 (5) ◽  
pp. 326-329
Author(s):  
Justiina Dahl ◽  
Peder Roberts ◽  
Lize-Marié van der Watt

AbstractAre similarities of temperature, snow and ice cover, and (certain) marine mammals sufficient to warrant both polar regions being considered a single object of study or governance? We argue that their treatment as a unit is an invitation to examine the motivations behind the choice to be polar rather than Arctic or Antarctic. For individuals such as James Clerk Ross or Roald Amundsen, logistical requirements and analogous goals facilitated careers spanning both the Arctic and the Antarctic. This trend continued through the 20th century as individual scientists studying phenomena such as glaciers, sea ice, or aurora defined their research as “polar” in nature. Organisations such as the Scott Polar Research Institute and Norwegian Polar Institute could draw on traditions of national exploration in both polar regions, while the Arctic and Antarctic Research Institute in St. Petersburg gained its southern mandate with the importance of the International Geophysical Year. By comparison, neither the Arctic Institute in Copenhagen nor the Argentine Antarctic Institute felt any need to become polar. The creation of polar identity is ultimately a matter of geopolitics, of the value states see in instruments and symbols that speak to polar rather than Arctic or Antarctic interests. In cases such as Finland’s icebreaker industry, a technological capability justified Antarctic interest even without any national research tradition. We conclude by asking whether there is anything more natural about the polar regions than there is about the concept of a “tripolar” world in which the high alpine regions form a natural unit along with the Arctic and Antarctic.


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