cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.4121/uuid:fd8cf390-8749-48e8-9eb1-d0a786e4eccf
title: IDRA weather radar measurements - day 2011-12-01

description: Radar range: standard. Max rain level: moderate rain. Parent item: IDRA weather radar measurements - month 2011-12 Measuring instrument: IDRA atmospheric radar in CESAR observatory, Cabauw IRCTR has built a high resolution radar system, IDRA (IRCTR Drizzle Radar), aimed at the detailed observation of the spatial and temporal distribution of rainfall and drizzle. The system was placed at the end of August 2007 on top of a 213 m high meteorological tower in the CESAR (Cabauw Experimental Site for Atmospheric Research) observatory in Cabauw, The Netherlands. This location has several advantages: In the first place, an increased sensitivity due to the reduction of the influence of ground clutter. Secondly, it allows direct observation of the horizontal distribution of low level clouds and fog. Finally, the presence of other instruments in the vicinity enhances the understanding of the physical processes in the atmosphere by synergistically combining their measurements. Data from other instruments at CESAR are available at {http://www.cesar-database.nl}. IDRA provides the horizontal distribution of reflectivity, mean Doppler velocity, Doppler spectrum width and polarimetric parameters like differential reflectivity, linear depolarization ratio or specific differential phase. The data collected is freely available to the scientific community.
DOI: 10.4121/uuid:feda5ebf-f5c1-42d7-a030-63c20a8b99ce
title: IDRA weather radar measurements - day 2011-12-17

description: Radar range: standard. Max rain level: moderate rain. Parent item: IDRA weather radar measurements - month 2011-12 Measuring instrument: IDRA atmospheric radar in CESAR observatory, Cabauw IRCTR has built a high resolution radar system, IDRA (IRCTR Drizzle Radar), aimed at the detailed observation of the spatial and temporal distribution of rainfall and drizzle. The system was placed at the end of August 2007 on top of a 213 m high meteorological tower in the CESAR (Cabauw Experimental Site for Atmospheric Research) observatory in Cabauw, The Netherlands. This location has several advantages: In the first place, an increased sensitivity due to the reduction of the influence of ground clutter. Secondly, it allows direct observation of the horizontal distribution of low level clouds and fog. Finally, the presence of other instruments in the vicinity enhances the understanding of the physical processes in the atmosphere by synergistically combining their measurements. Data from other instruments at CESAR are available at {http://www.cesar-database.nl}. IDRA provides the horizontal distribution of reflectivity, mean Doppler velocity, Doppler spectrum width and polarimetric parameters like differential reflectivity, linear depolarization ratio or specific differential phase. The data collected is freely available to the scientific community.
DOI: 10.4121/uuid:fee6cf06-af27-45d9-b81f-2b77eb774ba3
title: IDRA weather radar measurements - day 2011-12-16

description: Radar range: standard. Max rain level: moderate rain. Parent item: IDRA weather radar measurements - month 2011-12 Measuring instrument: IDRA atmospheric radar in CESAR observatory, Cabauw IRCTR has built a high resolution radar system, IDRA (IRCTR Drizzle Radar), aimed at the detailed observation of the spatial and temporal distribution of rainfall and drizzle. The system was placed at the end of August 2007 on top of a 213 m high meteorological tower in the CESAR (Cabauw Experimental Site for Atmospheric Research) observatory in Cabauw, The Netherlands. This location has several advantages: In the first place, an increased sensitivity due to the reduction of the influence of ground clutter. Secondly, it allows direct observation of the horizontal distribution of low level clouds and fog. Finally, the presence of other instruments in the vicinity enhances the understanding of the physical processes in the atmosphere by synergistically combining their measurements. Data from other instruments at CESAR are available at {http://www.cesar-database.nl}. IDRA provides the horizontal distribution of reflectivity, mean Doppler velocity, Doppler spectrum width and polarimetric parameters like differential reflectivity, linear depolarization ratio or specific differential phase. The data collected is freely available to the scientific community.
DOI: 10.4121/uuid:fefcdfee-37dc-435c-bd30-0a7746d4e2a6
title: IDRA weather radar measurements - day 2011-11-29

description: Radar range: standard. Max rain level: weak rain. Parent item: IDRA weather radar measurements - month 2011-11 Measuring instrument: IDRA atmospheric radar in CESAR observatory, Cabauw IRCTR has built a high resolution radar system, IDRA (IRCTR Drizzle Radar), aimed at the detailed observation of the spatial and temporal distribution of rainfall and drizzle. The system was placed at the end of August 2007 on top of a 213 m high meteorological tower in the CESAR (Cabauw Experimental Site for Atmospheric Research) observatory in Cabauw, The Netherlands. This location has several advantages: In the first place, an increased sensitivity due to the reduction of the influence of ground clutter. Secondly, it allows direct observation of the horizontal distribution of low level clouds and fog. Finally, the presence of other instruments in the vicinity enhances the understanding of the physical processes in the atmosphere by synergistically combining their measurements. Data from other instruments at CESAR are available at {http://www.cesar-database.nl}. IDRA provides the horizontal distribution of reflectivity, mean Doppler velocity, Doppler spectrum width and polarimetric parameters like differential reflectivity, linear depolarization ratio or specific differential phase. The data collected is freely available to the scientific community.
DOI: 10.4121/uuid:ff88d067-8404-403e-878f-dea80676b7a5
title: IDRA weather radar measurements - day 2011-12-03

description: Radar range: standard. Max rain level: moderate rain. Parent item: IDRA weather radar measurements - month 2011-12 Measuring instrument: IDRA atmospheric radar in CESAR observatory, Cabauw IRCTR has built a high resolution radar system, IDRA (IRCTR Drizzle Radar), aimed at the detailed observation of the spatial and temporal distribution of rainfall and drizzle. The system was placed at the end of August 2007 on top of a 213 m high meteorological tower in the CESAR (Cabauw Experimental Site for Atmospheric Research) observatory in Cabauw, The Netherlands. This location has several advantages: In the first place, an increased sensitivity due to the reduction of the influence of ground clutter. Secondly, it allows direct observation of the horizontal distribution of low level clouds and fog. Finally, the presence of other instruments in the vicinity enhances the understanding of the physical processes in the atmosphere by synergistically combining their measurements. Data from other instruments at CESAR are available at {http://www.cesar-database.nl}. IDRA provides the horizontal distribution of reflectivity, mean Doppler velocity, Doppler spectrum width and polarimetric parameters like differential reflectivity, linear depolarization ratio or specific differential phase. The data collected is freely available to the scientific community.
DOI: 10.4121/uuid:177969ea-0ca3-4090-a363-1fe37cd35017
title: STP algorithms and experimentation (software), version 2011-03-public

description: STP algorithms and experimentation (software), version 2011-03-public
DOI: 10.4121/uuid:158448c5-3133-4d3e-b1e9-91e7312a4878
title: Network instance Job shop, edition 2

description: STNs randomly generated in the SMT-LIB "diamonds" benchmark category. The benchmarks are DTP instances. STNs were generated from these by randomly selecting a literal from each clause. For each STN thus generated, the graph structure was maintained while modifying the weights of the constraint arcs such that at least one solution exists (i.e. the graph contains no negative cycles and the STN is consistent). This archive contains 400 graphs on 17–1321 vertices, 32–110220 edges, upper bound on treewidth 3–331. Parent item: Benchmark instances for experiments in ["Computing All-Pairs Shortest Paths by Leveraging Low Treewidth" (paper, 2012)]
DOI: 10.4121/uuid:776a266e-81c6-41ee-9d23-8c89d90b6992
title: STP algorithms and experimentation (software), version 2012-03-public

description: STP algorithms and experimentation (software), version 2012-03-public
DOI: 10.4121/uuid:5f6da46b-e2a2-4e05-a6cb-f22447393fb2
title: Network instance Scale-free; varying vertex count, bounded induced width, edition 2

description: Scale-free graphs generated following the Barabási-Albert method, then selected for induced width. The weights of the constraint arcs are set such that at least one solution exists (i.e. the graph contains no negative cycles and the STN is consistent). This archive contains 160 graphs on 250–1000 vertices, 2176–3330 edges, upper bound on treewidth 150–200. The scale-free density parameter for this selection is 3–15. Parent item: Benchmark instances for experiments in ["Computing All-Pairs Shortest Paths by Leveraging Low Treewidth" (paper, 2012)]
DOI: 10.4121/uuid:6cad8a1b-88db-4a64-97eb-b4f3f1a87047
title: Network instance Diamonds, edition 2

description: STNs randomly generated in the SMT-LIB "diamonds" benchmark category. The benchmarks are DTP instances. STNs were generated from these by randomly selecting a literal from each clause. For each STN thus generated, the graph structure was maintained while modifying the weights of the constraint arcs such that at least one solution exists (i.e. the graph contains no negative cycles and the STN is consistent). This archive contains 130 graphs on 111–2751 vertices, 111–2751 edges, upper bound on treewidth 2. Parent item: Benchmark instances for experiments in ["Computing All-Pairs Shortest Paths by Leveraging Low Treewidth" (paper, 2012)]
DOI: 10.4121/uuid:8f914d61-a9b6-4de0-9698-e0345dabb8e4
title: Network instance HTN, edition 2

description: Generated sibling-restricted STNs as they could result from a Hierarchical Task Network. Constraints exist between tasks and their children, and between sibling tasks; in addition, a limited number of "landmark" tasks is added which are exempt from this restriction. Branching factor 4–7; tree height 3–7; landmark ratio in [0,0.5]; probably of sibling edge in [0,0.5]. The weights of the constraint arcs are set such that at least one solution exists (i.e. the graph contains no negative cycles and the STN is consistent). This archive contains 121 graphs on 500–625 vertices, 748–1599 edges, upper bound on treewidth 2–128. Parent item: Benchmark instances for experiments in ["Computing All-Pairs Shortest Paths by Leveraging Low Treewidth" (paper, 2012)]
DOI: 10.4121/uuid:db232a00-6f0b-4df3-b56e-ade64077968c
title: Network instance Scale-free; constant vertex count, varying density, edition 2

description: Scale-free graphs generated following the Barabási-Albert method with 1000 vertices and density parameter varying from 2 to 80. The weights of the constraint arcs are set such that at least one solution exists (i.e. the graph contains no negative cycles and the STN is consistent). This archive contains 130 graphs on 1000 vertices, 1996–67360 edges, upper bound on treewidth 88–864. Parent item: Benchmark instances for experiments in ["Computing All-Pairs Shortest Paths by Leveraging Low Treewidth" (paper, 2012)]
DOI: 10.4121/uuid:fbe04397-94ba-4928-8111-be4026fc8b8d
title: Network instance New York, edition 2

description: Directed graphs with positive edge weights grown by breadth-first search from a random point in the New York City benchmark graphs as included in the 9th DIMACS Implementation Challenge (2005). This archive contains 170 graphs on 108–3906 vertices, 113–6422 edges, upper bound on treewidth 2–51. Parent item: Benchmark instances for experiments in ["Computing All-Pairs Shortest Paths by Leveraging Low Treewidth" (paper, 2012)]
DOI: 10.4121/uuid:fea4f033-6bc1-46d8-81f4-d17115304fdb
title: Network instance Chordal, fixed size, edition 2

description: Chordal graphs from a self-written generator. The weights of the constraint arcs are set such that at least one solution exists (i.e. the graph contains no negative cycles and the STN is consistent). This archive contains 250 graphs on 1000 vertices, 75840–499490 edges, treewidth 79–995. Parent item: Benchmark instances for experiments in ["Computing All-Pairs Shortest Paths by Leveraging Low Treewidth" (paper, 2012)]
DOI: 10.4121/uuid:30d29998-b054-4cf2-99e3-a34ee3397dab
title: The role of prenucleation clusters in surface-induced calcium phosphate crystallization - stage 5

description: Parent item: The role of prenucleation clusters in surface-induced calcium phosphate crystallization ACP formation is thought to proceed through prenucleation clusters. However, the role of such nanometre-sized clusters as building blocks2 for ACP has been debated for many years. Here we demonstrate that the surface-induced formation of apatite from simulated body fluid17, 18 starts with the aggregation of prenucleation clusters leading to the nucleation of ACP before the development of oriented apatite crystals. The data consists of separate sets for the five stages in this process. Datasets consist of original (mrc) data, the aligned (ali) data, reconstruction (rec) data, each of which may also be visualized with a video presentation.
DOI: 10.4121/uuid:3684ed02-038b-480f-8248-0f5752309dc1
title: The role of prenucleation clusters in surface-induced calcium phosphate crystallization - stage 1

description: Parent item: The role of prenucleation clusters in surface-induced calcium phosphate crystallization ACP formation is thought to proceed through prenucleation clusters. However, the role of such nanometre-sized clusters as building blocks2 for ACP has been debated for many years. Here we demonstrate that the surface-induced formation of apatite from simulated body fluid17, 18 starts with the aggregation of prenucleation clusters leading to the nucleation of ACP before the development of oriented apatite crystals. The data consists of separate sets for the five stages in this process. Datasets consist of original (mrc) data, the aligned (ali) data, reconstruction (rec) data, each of which may also be visualized with a video presentation.
DOI: 10.4121/uuid:827ebe59-3e6e-47c0-aaa3-5745e4e6d054
title: The role of prenucleation clusters in surface-induced calcium phosphate crystallization - stage 3

description: Parent item: The role of prenucleation clusters in surface-induced calcium phosphate crystallization ACP formation is thought to proceed through prenucleation clusters. However, the role of such nanometre-sized clusters as building blocks2 for ACP has been debated for many years. Here we demonstrate that the surface-induced formation of apatite from simulated body fluid17, 18 starts with the aggregation of prenucleation clusters leading to the nucleation of ACP before the development of oriented apatite crystals. The data consists of separate sets for the five stages in this process. Datasets consist of original (mrc) data, the aligned (ali) data, reconstruction (rec) data, each of which may also be visualized with a video presentation.
DOI: 10.4121/uuid:9ae3cd4e-9595-4b4f-bb93-1deafcfccf02
title: The role of prenucleation clusters in surface-induced calcium phosphate crystallization - stage 2

description: Parent item: The role of prenucleation clusters in surface-induced calcium phosphate crystallization ACP formation is thought to proceed through prenucleation clusters. However, the role of such nanometre-sized clusters as building blocks2 for ACP has been debated for many years. Here we demonstrate that the surface-induced formation of apatite from simulated body fluid17, 18 starts with the aggregation of prenucleation clusters leading to the nucleation of ACP before the development of oriented apatite crystals. The data consists of separate sets for the five stages in this process. Datasets consist of original (mrc) data, the aligned (ali) data, reconstruction (rec) data, each of which may also be visualized with a video presentation.
DOI: 10.4121/uuid:cabe50a1-cd91-466b-b4b7-26b363a1f896
title: The role of prenucleation clusters in surface-induced calcium phosphate crystallization - stage CaCl2 + K2HPO4

description: Parent item: The role of prenucleation clusters in surface-induced calcium phosphate crystallization ACP formation is thought to proceed through prenucleation clusters. However, the role of such nanometre-sized clusters as building blocks2 for ACP has been debated for many years. Here we demonstrate that the surface-induced formation of apatite from simulated body fluid17, 18 starts with the aggregation of prenucleation clusters leading to the nucleation of ACP before the development of oriented apatite crystals. The data consists of separate sets for the five stages in this process. Datasets consist of original (mrc) data, the aligned (ali) data, reconstruction (rec) data, each of which may also be visualized with a video presentation.
DOI: 10.4121/uuid:d6a45be8-d600-4972-a418-ecf57af295e4
title: The role of prenucleation clusters in surface-induced calcium phosphate crystallization - stage 4

description: Parent item: The role of prenucleation clusters in surface-induced calcium phosphate crystallization ACP formation is thought to proceed through prenucleation clusters. However, the role of such nanometre-sized clusters as building blocks2 for ACP has been debated for many years. Here we demonstrate that the surface-induced formation of apatite from simulated body fluid17, 18 starts with the aggregation of prenucleation clusters leading to the nucleation of ACP before the development of oriented apatite crystals. The data consists of separate sets for the five stages in this process. Datasets consist of original (mrc) data, the aligned (ali) data, reconstruction (rec) data, each of which may also be visualized with a video presentation.
DOI: 10.4121/uuid:00f2452c-8515-4511-8e48-732eaa5a29b7
title: IDRA weather radar measurements - day 2011-09-11

description: Radar range: standard. Max rain level: strong rain. Parent item: IDRA weather radar measurements - month 2011-09 Measuring instrument: IDRA atmospheric radar in CESAR observatory, Cabauw IRCTR has built a high resolution radar system, IDRA (IRCTR Drizzle Radar), aimed at the detailed observation of the spatial and temporal distribution of rainfall and drizzle. The system was placed at the end of August 2007 on top of a 213 m high meteorological tower in the CESAR (Cabauw Experimental Site for Atmospheric Research) observatory in Cabauw, The Netherlands. This location has several advantages: In the first place, an increased sensitivity due to the reduction of the influence of ground clutter. Secondly, it allows direct observation of the horizontal distribution of low level clouds and fog. Finally, the presence of other instruments in the vicinity enhances the understanding of the physical processes in the atmosphere by synergistically combining their measurements. Data from other instruments at CESAR are available at {http://www.cesar-database.nl}. IDRA provides the horizontal distribution of reflectivity, mean Doppler velocity, Doppler spectrum width and polarimetric parameters like differential reflectivity, linear depolarization ratio or specific differential phase. The data collected is freely available to the scientific community.
DOI: 10.4121/uuid:03f7b130-4dca-43ff-a452-49d427050783
title: IDRA weather radar measurements - day 2011-09-10

description: Radar range: standard. Max rain level: strong rain. Parent item: IDRA weather radar measurements - month 2011-09 Measuring instrument: IDRA atmospheric radar in CESAR observatory, Cabauw IRCTR has built a high resolution radar system, IDRA (IRCTR Drizzle Radar), aimed at the detailed observation of the spatial and temporal distribution of rainfall and drizzle. The system was placed at the end of August 2007 on top of a 213 m high meteorological tower in the CESAR (Cabauw Experimental Site for Atmospheric Research) observatory in Cabauw, The Netherlands. This location has several advantages: In the first place, an increased sensitivity due to the reduction of the influence of ground clutter. Secondly, it allows direct observation of the horizontal distribution of low level clouds and fog. Finally, the presence of other instruments in the vicinity enhances the understanding of the physical processes in the atmosphere by synergistically combining their measurements. Data from other instruments at CESAR are available at {http://www.cesar-database.nl}. IDRA provides the horizontal distribution of reflectivity, mean Doppler velocity, Doppler spectrum width and polarimetric parameters like differential reflectivity, linear depolarization ratio or specific differential phase. The data collected is freely available to the scientific community.
DOI: 10.4121/uuid:078e2079-3d67-475a-b511-84fa267219b7
title: IDRA weather radar measurements - day 2011-09-06

description: Radar range: standard. Max rain level: moderate rain. Parent item: IDRA weather radar measurements - month 2011-09 Measuring instrument: IDRA atmospheric radar in CESAR observatory, Cabauw IRCTR has built a high resolution radar system, IDRA (IRCTR Drizzle Radar), aimed at the detailed observation of the spatial and temporal distribution of rainfall and drizzle. The system was placed at the end of August 2007 on top of a 213 m high meteorological tower in the CESAR (Cabauw Experimental Site for Atmospheric Research) observatory in Cabauw, The Netherlands. This location has several advantages: In the first place, an increased sensitivity due to the reduction of the influence of ground clutter. Secondly, it allows direct observation of the horizontal distribution of low level clouds and fog. Finally, the presence of other instruments in the vicinity enhances the understanding of the physical processes in the atmosphere by synergistically combining their measurements. Data from other instruments at CESAR are available at {http://www.cesar-database.nl}. IDRA provides the horizontal distribution of reflectivity, mean Doppler velocity, Doppler spectrum width and polarimetric parameters like differential reflectivity, linear depolarization ratio or specific differential phase. The data collected is freely available to the scientific community.
DOI: 10.4121/uuid:07c75aa1-211e-4c73-b0b8-22e1670a9334
title: IDRA weather radar measurements - day 2011-10-15

description: Radar range: standard. Max rain level: weak rain. Parent item: IDRA weather radar measurements - month 2011-10 Measuring instrument: IDRA atmospheric radar in CESAR observatory, Cabauw IRCTR has built a high resolution radar system, IDRA (IRCTR Drizzle Radar), aimed at the detailed observation of the spatial and temporal distribution of rainfall and drizzle. The system was placed at the end of August 2007 on top of a 213 m high meteorological tower in the CESAR (Cabauw Experimental Site for Atmospheric Research) observatory in Cabauw, The Netherlands. This location has several advantages: In the first place, an increased sensitivity due to the reduction of the influence of ground clutter. Secondly, it allows direct observation of the horizontal distribution of low level clouds and fog. Finally, the presence of other instruments in the vicinity enhances the understanding of the physical processes in the atmosphere by synergistically combining their measurements. Data from other instruments at CESAR are available at {http://www.cesar-database.nl}. IDRA provides the horizontal distribution of reflectivity, mean Doppler velocity, Doppler spectrum width and polarimetric parameters like differential reflectivity, linear depolarization ratio or specific differential phase. The data collected is freely available to the scientific community.