Fukushima Nuclear Accident Recorded in Tibetan Plateau Snow Pits
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{"title"=>"Fukushima nuclear accident recorded in tibetan plateau snow pits", "type"=>"journal", "authors"=>[{"first_name"=>"Ninglian", "last_name"=>"Wang", "scopus_author_id"=>"35090697300"}, {"first_name"=>"Xiaobo", "last_name"=>"Wu", "scopus_author_id"=>"55715044700"}, {"first_name"=>"Natalie", "last_name"=>"Kehrwald", "scopus_author_id"=>"26028869800"}, {"first_name"=>"Zhen", "last_name"=>"Li", "scopus_author_id"=>"57184557300"}, {"first_name"=>"Quanlian", "last_name"=>"Li", "scopus_author_id"=>"56142847100"}, {"first_name"=>"Xi", "last_name"=>"Jiang", "scopus_author_id"=>"56142344000"}, {"first_name"=>"Jianchen", "last_name"=>"Pu", "scopus_author_id"=>"7102908972"}], "year"=>2015, "source"=>"PLoS ONE", "identifiers"=>{"pui"=>"602151097", "sgr"=>"84922638794", "scopus"=>"2-s2.0-84922638794", "doi"=>"10.1371/journal.pone.0116580", "issn"=>"19326203"}, "id"=>"1457f39f-f17b-3644-9589-16ae50373444", "abstract"=>"© 2015 Wang et al. The β radioactivity of snow-pit samples collected in the spring of 2011 on four Tibetan Plateau glaciers demonstrate a remarkable peak in each snow pit profile, with peaks about ten to tens of times higher than background levels. The timing of these peaks suggests that the high radioactivity resulted from the Fukushima nuclear accident that occurred on March 11, 2011 in eastern Japan. Fallout monitoring studies demonstrate that this radioactive material was transported by the westerlies across the middle latitudes of the Northern Hemisphere. The depth of the peak β radioactivity in each snow pit compared with observational precipitation records, suggests that the radioactive fallout reached the Tibetan Plateau and was deposited on glacier surfaces in late March 2011, or approximately 20 days after the nuclear accident. The radioactive fallout existed in the atmosphere over the Tibetan Plateau for about one month.", "link"=>"http://www.mendeley.com/research/fukushima-nuclear-accident-recorded-tibetan-plateau-snow-pits", "reader_count"=>6, "reader_count_by_academic_status"=>{"Researcher"=>2, "Student > Ph. D. Student"=>1, "Other"=>2, "Professor"=>1}, "reader_count_by_user_role"=>{"Researcher"=>2, "Student > Ph. D. Student"=>1, "Other"=>2, "Professor"=>1}, "reader_count_by_subject_area"=>{"Environmental Science"=>2, "Physics and Astronomy"=>1, "Earth and Planetary Sciences"=>3}, "reader_count_by_subdiscipline"=>{"Physics and Astronomy"=>{"Physics and Astronomy"=>1}, "Earth and Planetary Sciences"=>{"Earth and Planetary Sciences"=>3}, "Environmental Science"=>{"Environmental Science"=>2}}, "reader_count_by_country"=>{"China"=>1, "Japan"=>1, "India"=>1}, "group_count"=>0}

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Figshare

  • {"files"=>["https://ndownloader.figshare.com/files/1884124"], "description"=>"<p>Thin columns stand for daily precipitations while solid curves for their cumulative percentages calculated backward. Horizontal dashed lines represent the ratios of net accumulation amounts above the depths of the top and bottom limits of snow layer with the peak β radioactivity to the total net accumulation amount in the each study snow pit. The vertical dashed lines demonstrate the dates that the horizontal dashed lines intersect the curve of precipitation cumulative percentage. The dates determined using this technique correspond to the starting and ending dates of the deposition of Fukushima fallout on the surfaces of the Tibetan Plateau glaciers.</p>", "links"=>[], "tags"=>["fallout monitoring studies", "Tibetan Plateau", "snow pit profile", "Tibetan Plateau Snow Pits", "Tibetan Plateau glaciers", "accident", "radioactivity", "Fukushima Nuclear Accident Recorded"], "article_id"=>1303040, "categories"=>["Uncategorised"], "users"=>["Ninglian Wang", "Xiaobo Wu", "Natalie Kehrwald", "Zhen Li", "Quanlian Li", "Xi Jiang", "Jianchen Pu"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0116580.g006", "stats"=>{"downloads"=>2, "page_views"=>20, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Daily_precipitation_variations_and_their_cumulative_percentages_at_different_meteorological_stations_close_to_the_study_glaciers_in_the_Tibetan_Plateau_from_October_1_2010_to_the_sampling_dates_in_May_2011_/1303040", "title"=>"Daily precipitation variations and their cumulative percentages at different meteorological stations close to the study glaciers in the Tibetan Plateau from October 1, 2010 to the sampling dates in May 2011.", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2015-02-06 04:34:13"}
  • {"files"=>["https://ndownloader.figshare.com/files/1884118"], "description"=>"<p>Correlations between the β radioactivity and dust concentration in the Muztag and Tanggula ice cores from the Tibetan Plateau.</p>", "links"=>[], "tags"=>["fallout monitoring studies", "Tibetan Plateau", "snow pit profile", "Tibetan Plateau Snow Pits", "Tibetan Plateau glaciers", "accident", "radioactivity", "Fukushima Nuclear Accident Recorded"], "article_id"=>1303038, "categories"=>["Uncategorised"], "users"=>["Ninglian Wang", "Xiaobo Wu", "Natalie Kehrwald", "Zhen Li", "Quanlian Li", "Xi Jiang", "Jianchen Pu"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0116580.g005", "stats"=>{"downloads"=>0, "page_views"=>13, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Correlations_between_the_946_radioactivity_and_dust_concentration_in_the_Muztag_and_Tanggula_ice_cores_from_the_Tibetan_Plateau_/1303038", "title"=>"Correlations between the β radioactivity and dust concentration in the Muztag and Tanggula ice cores from the Tibetan Plateau.", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2015-02-06 04:34:13"}
  • {"files"=>["https://ndownloader.figshare.com/files/1884115"], "description"=>"<p>The very thin ice layers in snow pits (snow with ice lens) were formed by the refreezing of the small melt on the snow surface caused by the solar radiations in the cold accumulation period.</p>", "links"=>[], "tags"=>["fallout monitoring studies", "Tibetan Plateau", "snow pit profile", "Tibetan Plateau Snow Pits", "Tibetan Plateau glaciers", "accident", "radioactivity", "Fukushima Nuclear Accident Recorded"], "article_id"=>1303035, "categories"=>["Uncategorised"], "users"=>["Ninglian Wang", "Xiaobo Wu", "Natalie Kehrwald", "Zhen Li", "Quanlian Li", "Xi Jiang", "Jianchen Pu"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0116580.g002", "stats"=>{"downloads"=>0, "page_views"=>28, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Stratigraphic_profiles_of_the_snow_pits_on_the_Tibetan_Plateau_study_glaciers_in_spring_2011_/1303035", "title"=>"Stratigraphic profiles of the snow pits on the Tibetan Plateau study glaciers in spring 2011.", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2015-02-06 04:34:13"}
  • {"files"=>["https://ndownloader.figshare.com/files/1884132"], "description"=>"<p>Locations of snow pits and sampling dates on the different Tibetan Plateau glaciers.</p>", "links"=>[], "tags"=>["fallout monitoring studies", "Tibetan Plateau", "snow pit profile", "Tibetan Plateau Snow Pits", "Tibetan Plateau glaciers", "accident", "radioactivity", "Fukushima Nuclear Accident Recorded"], "article_id"=>1303043, "categories"=>["Uncategorised"], "users"=>["Ninglian Wang", "Xiaobo Wu", "Natalie Kehrwald", "Zhen Li", "Quanlian Li", "Xi Jiang", "Jianchen Pu"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0116580.t001", "stats"=>{"downloads"=>4, "page_views"=>15, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Locations_of_snow_pits_and_sampling_dates_on_the_different_Tibetan_Plateau_glaciers_/1303043", "title"=>"Locations of snow pits and sampling dates on the different Tibetan Plateau glaciers.", "pos_in_sequence"=>0, "defined_type"=>3, "published_date"=>"2015-02-06 04:34:13"}
  • {"files"=>["https://ndownloader.figshare.com/files/1884131"], "description"=>"<p>They were computed by using the HYSPLIT model and the GDAS meteorological data (<a href=\"http://www.arl.noaa.gov/HYSPLIT.php\" target=\"_blank\">http://www.arl.noaa.gov/HYSPLIT.php</a>). Panel (a) represents the status as for the Gurenhekou Glacier, (b) for the Dongkemadi Glacier, (c) for the Yuzhufeng Glacier, and (d) for the Muztag Glacier.</p>", "links"=>[], "tags"=>["fallout monitoring studies", "Tibetan Plateau", "snow pit profile", "Tibetan Plateau Snow Pits", "Tibetan Plateau glaciers", "accident", "radioactivity", "Fukushima Nuclear Accident Recorded"], "article_id"=>1303042, "categories"=>["Uncategorised"], "users"=>["Ninglian Wang", "Xiaobo Wu", "Natalie Kehrwald", "Zhen Li", "Quanlian Li", "Xi Jiang", "Jianchen Pu"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0116580.g007", "stats"=>{"downloads"=>0, "page_views"=>21, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_The_backward_air_parcel_trajectories_at_the_heights_of_1000_m_2000_m_and_4500_m_above_ground_level_of_the_study_sites_at_about_the_starting_dates_of_the_Fukushima_fallout_deposition_on_the_Tibetan_Plateau_glaciers_/1303042", "title"=>"The backward air parcel trajectories at the heights of 1000 m, 2000 m and 4500 m above ground level of the study sites at about the starting dates of the Fukushima fallout deposition on the Tibetan Plateau glaciers.", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2015-02-06 04:34:13"}
  • {"files"=>["https://ndownloader.figshare.com/files/1884117"], "description"=>"<p>Profiles of the β radioactivities recorded in the four study snow pits and two Tibetan Plateau ice cores.</p>", "links"=>[], "tags"=>["fallout monitoring studies", "Tibetan Plateau", "snow pit profile", "Tibetan Plateau Snow Pits", "Tibetan Plateau glaciers", "accident", "radioactivity", "Fukushima Nuclear Accident Recorded"], "article_id"=>1303037, "categories"=>["Uncategorised"], "users"=>["Ninglian Wang", "Xiaobo Wu", "Natalie Kehrwald", "Zhen Li", "Quanlian Li", "Xi Jiang", "Jianchen Pu"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0116580.g004", "stats"=>{"downloads"=>0, "page_views"=>9, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Profiles_of_the_946_radioactivities_recorded_in_the_four_study_snow_pits_and_two_Tibetan_Plateau_ice_cores_/1303037", "title"=>"Profiles of the β radioactivities recorded in the four study snow pits and two Tibetan Plateau ice cores.", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2015-02-06 04:34:13"}
  • {"files"=>["https://ndownloader.figshare.com/files/1884116"], "description"=>"<p>Variations of δ<sup>18</sup>O with depth in the snow pits on the study glaciers in the Tibetan Plateau.</p>", "links"=>[], "tags"=>["fallout monitoring studies", "Tibetan Plateau", "snow pit profile", "Tibetan Plateau Snow Pits", "Tibetan Plateau glaciers", "accident", "radioactivity", "Fukushima Nuclear Accident Recorded"], "article_id"=>1303036, "categories"=>["Uncategorised"], "users"=>["Ninglian Wang", "Xiaobo Wu", "Natalie Kehrwald", "Zhen Li", "Quanlian Li", "Xi Jiang", "Jianchen Pu"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0116580.g003", "stats"=>{"downloads"=>0, "page_views"=>11, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Variations_of_18_O_with_depth_in_the_snow_pits_on_the_study_glaciers_in_the_Tibetan_Plateau_/1303036", "title"=>"Variations of δ<sup>18</sup>O with depth in the snow pits on the study glaciers in the Tibetan Plateau.", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2015-02-06 04:34:13"}
  • {"files"=>["https://ndownloader.figshare.com/files/1884113"], "description"=>"<p>Locations of the study glaciers and their adjacent meteorological stations on the Tibetan Plateau.</p>", "links"=>[], "tags"=>["fallout monitoring studies", "Tibetan Plateau", "snow pit profile", "Tibetan Plateau Snow Pits", "Tibetan Plateau glaciers", "accident", "radioactivity", "Fukushima Nuclear Accident Recorded"], "article_id"=>1303033, "categories"=>["Uncategorised"], "users"=>["Ninglian Wang", "Xiaobo Wu", "Natalie Kehrwald", "Zhen Li", "Quanlian Li", "Xi Jiang", "Jianchen Pu"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0116580.g001", "stats"=>{"downloads"=>0, "page_views"=>11, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Locations_of_the_study_glaciers_and_their_adjacent_meteorological_stations_on_the_Tibetan_Plateau_/1303033", "title"=>"Locations of the study glaciers and their adjacent meteorological stations on the Tibetan Plateau.", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2015-02-06 04:34:13"}
  • {"files"=>["https://ndownloader.figshare.com/files/1884134", "https://ndownloader.figshare.com/files/1884135"], "description"=>"<div><p>The β radioactivity of snow-pit samples collected in the spring of 2011 on four Tibetan Plateau glaciers demonstrate a remarkable peak in each snow pit profile, with peaks about ten to tens of times higher than background levels. The timing of these peaks suggests that the high radioactivity resulted from the Fukushima nuclear accident that occurred on March 11, 2011 in eastern Japan. Fallout monitoring studies demonstrate that this radioactive material was transported by the westerlies across the middle latitudes of the Northern Hemisphere. The depth of the peak β radioactivity in each snow pit compared with observational precipitation records, suggests that the radioactive fallout reached the Tibetan Plateau and was deposited on glacier surfaces in late March 2011, or approximately 20 days after the nuclear accident. The radioactive fallout existed in the atmosphere over the Tibetan Plateau for about one month.</p></div>", "links"=>[], "tags"=>["fallout monitoring studies", "Tibetan Plateau", "snow pit profile", "Tibetan Plateau Snow Pits", "Tibetan Plateau glaciers", "accident", "radioactivity", "Fukushima Nuclear Accident Recorded"], "article_id"=>1303045, "categories"=>["Uncategorised"], "users"=>["Ninglian Wang", "Xiaobo Wu", "Natalie Kehrwald", "Zhen Li", "Quanlian Li", "Xi Jiang", "Jianchen Pu"], "doi"=>["https://dx.doi.org/10.1371/journal.pone.0116580.s001", "https://dx.doi.org/10.1371/journal.pone.0116580.s002"], "stats"=>{"downloads"=>4, "page_views"=>17, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Fukushima_Nuclear_Accident_Recorded_in_Tibetan_Plateau_Snow_Pits_/1303045", "title"=>"Fukushima Nuclear Accident Recorded in Tibetan Plateau Snow Pits", "pos_in_sequence"=>0, "defined_type"=>4, "published_date"=>"2015-02-06 04:34:13"}
  • {"files"=>["https://ndownloader.figshare.com/files/1884133"], "description"=>"<p>* The date (year.month.day) outside of the parenthesis is the optimal estimate time by using the net accumulation ratio along with the cumulative precipitation percentage curve. The dates (month.day-month.day) in the parentheses are the possible time period estimated by the net accumulation ratio along with the two adjacent cumulative precipitation percentages, and the large time span estimated on the Muztag Glacier might be resulted from the application of the meteorological data from the Mangya Station which is far from the glacier (there is no other stations closer to the glacier than the Mangya Station).</p><p>Time period of Japan Fukushima fallout deposited on the glaciers in the Tibetan Plateau estimated by the positions of the peak β radioactivaties in the study snow pits.</p>", "links"=>[], "tags"=>["fallout monitoring studies", "Tibetan Plateau", "snow pit profile", "Tibetan Plateau Snow Pits", "Tibetan Plateau glaciers", "accident", "radioactivity", "Fukushima Nuclear Accident Recorded"], "article_id"=>1303044, "categories"=>["Uncategorised"], "users"=>["Ninglian Wang", "Xiaobo Wu", "Natalie Kehrwald", "Zhen Li", "Quanlian Li", "Xi Jiang", "Jianchen Pu"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0116580.t002", "stats"=>{"downloads"=>3, "page_views"=>25, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Time_period_of_Japan_Fukushima_fallout_deposited_on_the_glaciers_in_the_Tibetan_Plateau_estimated_by_the_positions_of_the_peak_946_radioactivaties_in_the_study_snow_pits_/1303044", "title"=>"Time period of Japan Fukushima fallout deposited on the glaciers in the Tibetan Plateau estimated by the positions of the peak β radioactivaties in the study snow pits.", "pos_in_sequence"=>0, "defined_type"=>3, "published_date"=>"2015-02-06 04:34:13"}

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{"start_date"=>"2015-01-01T00:00:00Z", "end_date"=>"2015-12-31T00:00:00Z", "subject_areas"=>[]}
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