interactive data language idl version 8.2 Search Results


idl (interactive data language)  (RSI Inc)
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Idl (Interactive Data Language), supplied by RSI Inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
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interactive data language version 8.6  (Harris Geospatial Solutions)
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Interactive Data Language Version 8.6, supplied by Harris Geospatial Solutions, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
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custom interactive data language (idl) programme  (Harris Geospatial Solutions)
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Custom Interactive Data Language (Idl) Programme, supplied by Harris Geospatial Solutions, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
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cchips/idl software  (RSI Inc)
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Cchips/Idl Software, supplied by RSI Inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
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interactive data language idl  (Exelis Inc)
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Exelis Inc interactive data language idl
Interactive Data Language Idl, supplied by Exelis Inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
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interactive data language idl - by Bioz Stars, 2026-06
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idl (interactive data language)  (ITT Industries Inc)
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ITT Industries Inc idl (interactive data language)
Idl (Interactive Data Language), supplied by ITT Industries Inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
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interactive data language idl 8.4  (Harris Geospatial Solutions)
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Harris Geospatial Solutions interactive data language idl 8.4
Interactive Data Language Idl 8.4, supplied by Harris Geospatial Solutions, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
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idl program  (RSI Inc)
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RSI Inc idl program
Idl Program, supplied by RSI Inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
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computer software idl  (Harris Geospatial Solutions)
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Computer Software Idl, supplied by Harris Geospatial Solutions, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
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idl  (Harris Geospatial Solutions)
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Harris Geospatial Solutions idl
Sea ice drift trajectories leading to the 60°E section and δ 18 O isotopic composition (filled symbols) and salinity (open symbols) in sea ice at this section. Backward drift trajectories from the 60°E section show the sea ice formation areas, i.e. off shore within the Laptev Sea and in the coastal polynya areas. Trajectories were calculated based on a combination of sea ice motion and concentration products from passive microwave satellite data. The colour of the end node indicates the source area of sampled sea ice. Trajectories with red end nodes were formed in polynyas, namely the New Siberian (NS) Polynya, Taymyr (T) Polynya, Northeastern Taymyr (NET) Polynya and East Severnaya Zemlya (ESZ) Polynya. Grey end nodes refer to trajectories that were formed during freeze-up further offshore. The colour coding of the start node characterizes the month of formation (primarily October) of the individual trajectories. The δ 18 O ice isotopic composition reflects the δ 18 O composition of the water column from which each segment of the ice core was formed. Light values below about −4‰ indicate formation in coastal polynyas while values above −2‰ indicate freeze-up formation offshore. Salinity of the ice cores is in all cases below 4. The map is generated with <t>IDL</t> (Interactive Data <t>Langue),</t> <t>software</t> for analysis and visualization of data provided by Harris Geospatial Solutions ( http://www.harrisgeospatial.com ).
Idl, supplied by Harris Geospatial Solutions, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/result/idl/product/Harris Geospatial Solutions
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idl - by Bioz Stars, 2026-06
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idl 6.3  (RSI Inc)
90
RSI Inc idl 6.3
Sea ice drift trajectories leading to the 60°E section and δ 18 O isotopic composition (filled symbols) and salinity (open symbols) in sea ice at this section. Backward drift trajectories from the 60°E section show the sea ice formation areas, i.e. off shore within the Laptev Sea and in the coastal polynya areas. Trajectories were calculated based on a combination of sea ice motion and concentration products from passive microwave satellite data. The colour of the end node indicates the source area of sampled sea ice. Trajectories with red end nodes were formed in polynyas, namely the New Siberian (NS) Polynya, Taymyr (T) Polynya, Northeastern Taymyr (NET) Polynya and East Severnaya Zemlya (ESZ) Polynya. Grey end nodes refer to trajectories that were formed during freeze-up further offshore. The colour coding of the start node characterizes the month of formation (primarily October) of the individual trajectories. The δ 18 O ice isotopic composition reflects the δ 18 O composition of the water column from which each segment of the ice core was formed. Light values below about −4‰ indicate formation in coastal polynyas while values above −2‰ indicate freeze-up formation offshore. Salinity of the ice cores is in all cases below 4. The map is generated with <t>IDL</t> (Interactive Data <t>Langue),</t> <t>software</t> for analysis and visualization of data provided by Harris Geospatial Solutions ( http://www.harrisgeospatial.com ).
Idl 6.3, supplied by RSI Inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/result/idl 6.3/product/RSI Inc
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idl 6.3 - by Bioz Stars, 2026-06
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custom software written in idl  (Harris Geospatial Solutions)
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Harris Geospatial Solutions custom software written in idl
Sea ice drift trajectories leading to the 60°E section and δ 18 O isotopic composition (filled symbols) and salinity (open symbols) in sea ice at this section. Backward drift trajectories from the 60°E section show the sea ice formation areas, i.e. off shore within the Laptev Sea and in the coastal polynya areas. Trajectories were calculated based on a combination of sea ice motion and concentration products from passive microwave satellite data. The colour of the end node indicates the source area of sampled sea ice. Trajectories with red end nodes were formed in polynyas, namely the New Siberian (NS) Polynya, Taymyr (T) Polynya, Northeastern Taymyr (NET) Polynya and East Severnaya Zemlya (ESZ) Polynya. Grey end nodes refer to trajectories that were formed during freeze-up further offshore. The colour coding of the start node characterizes the month of formation (primarily October) of the individual trajectories. The δ 18 O ice isotopic composition reflects the δ 18 O composition of the water column from which each segment of the ice core was formed. Light values below about −4‰ indicate formation in coastal polynyas while values above −2‰ indicate freeze-up formation offshore. Salinity of the ice cores is in all cases below 4. The map is generated with <t>IDL</t> (Interactive Data <t>Langue),</t> <t>software</t> for analysis and visualization of data provided by Harris Geospatial Solutions ( http://www.harrisgeospatial.com ).
Custom Software Written In Idl, supplied by Harris Geospatial Solutions, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/result/custom software written in idl/product/Harris Geospatial Solutions
Average 90 stars, based on 1 article reviews
custom software written in idl - by Bioz Stars, 2026-06
90/100 stars
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Image Search Results


Sea ice drift trajectories leading to the 60°E section and δ 18 O isotopic composition (filled symbols) and salinity (open symbols) in sea ice at this section. Backward drift trajectories from the 60°E section show the sea ice formation areas, i.e. off shore within the Laptev Sea and in the coastal polynya areas. Trajectories were calculated based on a combination of sea ice motion and concentration products from passive microwave satellite data. The colour of the end node indicates the source area of sampled sea ice. Trajectories with red end nodes were formed in polynyas, namely the New Siberian (NS) Polynya, Taymyr (T) Polynya, Northeastern Taymyr (NET) Polynya and East Severnaya Zemlya (ESZ) Polynya. Grey end nodes refer to trajectories that were formed during freeze-up further offshore. The colour coding of the start node characterizes the month of formation (primarily October) of the individual trajectories. The δ 18 O ice isotopic composition reflects the δ 18 O composition of the water column from which each segment of the ice core was formed. Light values below about −4‰ indicate formation in coastal polynyas while values above −2‰ indicate freeze-up formation offshore. Salinity of the ice cores is in all cases below 4. The map is generated with IDL (Interactive Data Langue), software for analysis and visualization of data provided by Harris Geospatial Solutions ( http://www.harrisgeospatial.com ).

Journal: Scientific Reports

Article Title: The Transpolar Drift conveys methane from the Siberian Shelf to the central Arctic Ocean

doi: 10.1038/s41598-018-22801-z

Figure Lengend Snippet: Sea ice drift trajectories leading to the 60°E section and δ 18 O isotopic composition (filled symbols) and salinity (open symbols) in sea ice at this section. Backward drift trajectories from the 60°E section show the sea ice formation areas, i.e. off shore within the Laptev Sea and in the coastal polynya areas. Trajectories were calculated based on a combination of sea ice motion and concentration products from passive microwave satellite data. The colour of the end node indicates the source area of sampled sea ice. Trajectories with red end nodes were formed in polynyas, namely the New Siberian (NS) Polynya, Taymyr (T) Polynya, Northeastern Taymyr (NET) Polynya and East Severnaya Zemlya (ESZ) Polynya. Grey end nodes refer to trajectories that were formed during freeze-up further offshore. The colour coding of the start node characterizes the month of formation (primarily October) of the individual trajectories. The δ 18 O ice isotopic composition reflects the δ 18 O composition of the water column from which each segment of the ice core was formed. Light values below about −4‰ indicate formation in coastal polynyas while values above −2‰ indicate freeze-up formation offshore. Salinity of the ice cores is in all cases below 4. The map is generated with IDL (Interactive Data Langue), software for analysis and visualization of data provided by Harris Geospatial Solutions ( http://www.harrisgeospatial.com ).

Article Snippet: The map is generated with IDL (Interactive Data Langue), software for analysis and visualization of data provided by Harris Geospatial Solutions ( http://www.harrisgeospatial.com ).

Techniques: Concentration Assay, Generated, Software