cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.14272/fdbvyqicxlagqp-ccezhusrsa-n/nmr/1h/cdcl3/400
title: NMR/1H/CDCL3/400 ((E)-3,3-diisopropyl-1-(4-methoxyphenyl)triaz-1-ene)

description: This is a dataset.
DOI: 10.14272/fdbvyqicxlagqp-ccezhusrsa-n/tlc
title: TLC ((E)-3,3-diisopropyl-1-(4-methoxyphenyl)triaz-1-ene)

description: This is a dataset.
DOI: 10.14272/khgijsnpmcjuju-foclmdbbsa-n
title: (E)-1-(2,6-dimethylphenyl)-3,3-diisopropyltriaz-1-ene

description: This is a molecule publication.
DOI: 10.14272/khgijsnpmcjuju-foclmdbbsa-n/nmr/1h/cdcl3/400
title: NMR/1H/CDCL3/400 ((E)-1-(2,6-dimethylphenyl)-3,3-diisopropyltriaz-1-ene)

description: This is a dataset.
DOI: 10.14272/khgijsnpmcjuju-foclmdbbsa-n/ir
title: IR ((E)-1-(2,6-dimethylphenyl)-3,3-diisopropyltriaz-1-ene)

description: This is a dataset.
DOI: 10.14272/khgijsnpmcjuju-foclmdbbsa-n/mass/ei
title: Mass/EI ((E)-1-(2,6-dimethylphenyl)-3,3-diisopropyltriaz-1-ene)

description: This is a dataset.
DOI: 10.14272/khgijsnpmcjuju-foclmdbbsa-n/nmr/13c/cdcl3/100
title: NMR/13C/CDCL3/100 ((E)-1-(2,6-dimethylphenyl)-3,3-diisopropyltriaz-1-ene)

description: This is a dataset.
DOI: 10.14272/khgijsnpmcjuju-foclmdbbsa-n/tlc
title: TLC ((E)-1-(2,6-dimethylphenyl)-3,3-diisopropyltriaz-1-ene)

description: This is a dataset.
DOI: 10.5255/ukda-sn-7037-3
title: Quarterly Labour Force Survey, January - March, 2012
DOI: 10.14272/nvfrowunuwgjrs-ccezhusrsa-n
title: (E)-1-(4-chlorophenyl)-3,3-diisopropyltriaz-1-ene

description: This is a molecule publication.
DOI: 10.14272/nvfrowunuwgjrs-ccezhusrsa-n/nmr/1h/cdcl3/400
title: NMR/1H/CDCL3/400 ((E)-1-(4-chlorophenyl)-3,3-diisopropyltriaz-1-ene)

description: This is a dataset.
DOI: 10.14272/ykqkzhfkrzjocg-wukndpdisa-n/ir
title: IR ((E)-ethyl 4-(3,3-diisopropyltriaz-1-en-1-yl)benzoate)

description: This is a dataset.
DOI: 10.14272/ykqkzhfkrzjocg-wukndpdisa-n/mass/ei
title: Mass/EI ((E)-ethyl 4-(3,3-diisopropyltriaz-1-en-1-yl)benzoate)

description: This is a dataset.
DOI: 10.14272/ykqkzhfkrzjocg-wukndpdisa-n/nmr/13c/cdcl3/100
title: NMR/13C/CDCL3/100 ((E)-ethyl 4-(3,3-diisopropyltriaz-1-en-1-yl)benzoate)

description: This is a dataset.
DOI: 10.14272/ykqkzhfkrzjocg-wukndpdisa-n/nmr/1h/cdcl3/400
title: NMR/1H/CDCL3/400 ((E)-ethyl 4-(3,3-diisopropyltriaz-1-en-1-yl)benzoate)

description: This is a dataset.
DOI: 10.14272/ykqkzhfkrzjocg-wukndpdisa-n/tlc
title: TLC ((E)-ethyl 4-(3,3-diisopropyltriaz-1-en-1-yl)benzoate)

description: This is a dataset.
DOI: 10.14272/nvfrowunuwgjrs-ccezhusrsa-n/ir
title: IR ((E)-1-(4-chlorophenyl)-3,3-diisopropyltriaz-1-ene)

description: This is a dataset.
DOI: 10.14272/nvfrowunuwgjrs-ccezhusrsa-n/mass/ei
title: Mass/EI ((E)-1-(4-chlorophenyl)-3,3-diisopropyltriaz-1-ene)

description: This is a dataset.
DOI: 10.14272/nvfrowunuwgjrs-ccezhusrsa-n/nmr/13c/cdcl3/100
title: NMR/13C/CDCL3/100 ((E)-1-(4-chlorophenyl)-3,3-diisopropyltriaz-1-ene)

description: This is a dataset.
DOI: 10.14272/nvfrowunuwgjrs-ccezhusrsa-n/tlc
title: TLC ((E)-1-(4-chlorophenyl)-3,3-diisopropyltriaz-1-ene)

description: This is a dataset.
DOI: 10.6073/pasta/0aeb289ed1a7e192013c7bfc322807bd
title: Anaktuvuk River Burn Eddy Flux Measurements, 2012 Unburned Site, North Slope Alaska
DOI: 10.6073/pasta/c6f90d6b3a399015756d49fa19336d40
title: Anaktuvuk River Burn Eddy Flux Measurements, 2012 Severe Burn Site, North Slope Alaska
DOI: 10.6073/pasta/ca5fe06b5459ea188e4cf6daf77b8a05
title: Anaktuvuk River Burn Eddy Flux Measurements, 2012 Moderate Burn Site, North Slope Alaska
DOI: 10.14272/iegzewacyogsrs-uhfffaoysa-n
title: 9-(tert-Butyl)-1,5-dithiaspiro[5.5]undecane

description: This is a molecule publication.
DOI: 10.14272/iegzewacyogsrs-uhfffaoysa-n/nmr/13c/cdcl3/100
title: NMR/13C/CDCL3/100 (9-(tert-Butyl)-1,5-dithiaspiro[5.5]undecane)

description: This is a dataset.
DOI: 10.14272/iegzewacyogsrs-uhfffaoysa-n/nmr/1h/cdcl3/400
title: NMR/1H/CDCL3/400 (9-(tert-Butyl)-1,5-dithiaspiro[5.5]undecane)

description: This is a dataset.
DOI: 10.14272/iegzewacyogsrs-uhfffaoysa-n/ir
title: IR (9-(tert-Butyl)-1,5-dithiaspiro[5.5]undecane)

description: This is a dataset.
DOI: 10.14272/iegzewacyogsrs-uhfffaoysa-n/mass/ei
title: Mass/EI (9-(tert-Butyl)-1,5-dithiaspiro[5.5]undecane)

description: This is a dataset.
DOI: 10.14272/iegzewacyogsrs-uhfffaoysa-n/tlc
title: TLC (9-(tert-Butyl)-1,5-dithiaspiro[5.5]undecane)

description: This is a dataset.
DOI: 10.6073/pasta/1cef9a9725c8158b34e3c162239c242f
title: LiDAR data (August 2008)  for the Andrews Experimental Forest and Willamette National Forest study areas
DOI: 10.4231/d3d21rj44
title: Seismic earth pressures in a deep basement wall on dry sand (NW01)

description: The seismic response of a 45 ft basement was studied the centrifuge. The 2 story basement was built on a 1/36 scale. The walls were built with 0.5in aluminum plates and
DOI: 10.4225/08/5278358767c0b
title: Environmental Plantings Inventory

description: Inventory (tree and shrub heights and stem diameters) for mixed-species environmental plantings collected for estimation of biomass carbon.
DOI: 10.4225/08/52787b5f87a72
title: Modelled seabed response to possible climate change scenarios over the next 50 years in the Australian Southwest - High Energy scenario datasets with Sedsim input files and output files

description: Using data from ocean forecast models, field observations and seabed sampling we ran a numerical sediment transport model to estimate the Australian Shelf seabed evolution under three climate change scenarios. This data collection is for the High Energy climate change scenario of:  
    highest rainfall,
    highest sediment load,
    highest outflow, and
    highest oceanographic conditions,
    maximum sea level rise in next 50 years.

In this study, the interaction of seabed sediment types and hydrodynamic forces in the southwestern region has been investigated using a state-of-the-art numerical model, Sedsim. The simulation area  for this collection covers southwest Australia continental shelf and abyssal basins which include the Rottnest Shelf, the Perth Canyon, the Albany Canyons, the Great Australian Bight, the Lincoln Shelf, the Spencer Gulf, the Gulf St Vincent, and part of the Lacepede Shelf.

The model uses the known grain-size distribution of the present-day seabed based on a comprehensive analysis of currently available seabed data Information available from this data source includes grainsize, mud content, rock exposure, and estimates of critical seabed shear stress. This sediment layer is incorporated in the latest high-resolution (0.0025°) seabed bathymetry obtained from the Australian National Oceans Office (NOO). The seabed topography and present-day sediment layer are represented by a 566 (columns) by 550 (rows) grid with a spatial resolution of 2.1 km. The environmental forcing factors considered in the present model are sediment-laden river flows and turbidity currents, waves, tides, wind-driven currents, sea level change, submarine slope failure and carbonate sediment production.
DOI: 10.4225/08/52787bc31c83f
title: Modelled seabed response to possible climate change scenarios over the next 50 years in the Australian Southwest - Stationary scenario datasets with Sedsim input files and output files

description: Using data from ocean forecast models, field observations and seabed sampling we ran a numerical sediment transport model to estimate the Australian Shelf seabed evolution under three climate change scenarios. This data collection is for the Stationary climate change scenario in which the present climate continues for next 50 years.

In this study, the interaction of seabed sediment types and hydrodynamic forces in the southwestern region has been investigated using a state-of-the-art numerical model, Sedsim. The simulation area  for this collection covers southwest Australia continental shelf and abyssal basins which include the Rottnest Shelf, the Perth Canyon, the Albany Canyons, the Great Australian Bight, the Lincoln Shelf, the Spencer Gulf, the Gulf St Vincent, and part of the Lacepede Shelf.

The model uses the known grain-size distribution of the present-day seabed based on a comprehensive analysis of currently available seabed data Information available from this data source includes grainsize, mud content, rock exposure, and estimates of critical seabed shear stress. This sediment layer is incorporated in the latest high-resolution (0.0025°) seabed bathymetry obtained from the Australian National Oceans Office (NOO). The seabed topography and present-day sediment layer are represented by a 566 (columns) by 550 (rows) grid with a spatial resolution of 2.1 km. The environmental forcing factors considered in the present model are sediment-laden river flows and turbidity currents, waves, tides, wind-driven currents, sea level change, submarine slope failure and carbonate sediment production.
DOI: 10.4225/08/52787c1404d13
title: Modelled seabed response to possible climate change scenarios over the next 50 years in the Australian Southeast - Low Energy scenario datasets with Sedsim input files and output files

description: Using data from ocean forecast models, field observations and seabed sampling we ran a numerical sediment transport model to estimate the Australian Shelf seabed evolution under three climate change scenarios. This data collection is for the Low Energy climate change scenario of:  
    lowest rainfall,
    lowest sediment load,
    lowest outflow, and
    El-Niño year oceanographic conditions,
    no sea level rise in next 50 years.

In this study, the interaction of seabed sediment types and hydrodynamic forces in the southeastern region has been investigated using a state-of-the-art numerical model, Sedsim. The simulation area  for this collection covers the south-eastern Australian continental shelf and abyssal basins, including Bass Strait, the Tasman Sea, and the Tasmanian coast, as well as part of the South Australian and New South Wales coasts.

The model uses the known grain-size distribution of the present-day seabed based on a comprehensive analysis of currently available seabed data Information available from this data source includes grainsize, mud content, rock exposure, and estimates of critical seabed shear stress. This sediment layer is incorporated in the latest high-resolution (0.0025°) seabed bathymetry obtained from the Australian National Oceans Office (NOO). The seabed topography and present-day sediment layer are represented by a 566 (columns) by 550 (rows) grid with a spatial resolution of 2.1 km. The environmental forcing factors considered in the present model are sediment-laden river flows and turbidity currents, waves, tides, wind-driven currents, sea level change, submarine slope failure and carbonate sediment production.
DOI: 10.4225/08/52787c3ed1b8c
title: Modelled seabed response to possible climate change scenarios over the next 50 years in the Australian Southwest - Low Energy scenario datasets with Sedsim input files and output files

description: Using data from ocean forecast models, field observations and seabed sampling we ran a numerical sediment transport model to estimate the Australian Shelf seabed evolution under three climate change scenarios. This data collection is for the Low Energy climate change scenario of:  
    lowest rainfall,
    lowest sediment load,
    lowest outflow, and	
    El-Niño year oceanographic conditions,
    no sea level rise in next 50 years.

In this study, the interaction of seabed sediment types and hydrodynamic forces in the southwestern region has been investigated using a state-of-the-art numerical model, Sedsim. The simulation area  for this collection covers southwest Australia continental shelf and abyssal basins which include the Rottnest Shelf, the Perth Canyon, the Albany Canyons, the Great Australian Bight, the Lincoln Shelf, the Spencer Gulf, the Gulf St Vincent, and part of the Lacepede Shelf.

The model uses the known grain-size distribution of the present-day seabed based on a comprehensive analysis of currently available seabed data Information available from this data source includes grainsize, mud content, rock exposure, and estimates of critical seabed shear stress. This sediment layer is incorporated in the latest high-resolution (0.0025°) seabed bathymetry obtained from the Australian National Oceans Office (NOO). The seabed topography and present-day sediment layer are represented by a 566 (columns) by 550 (rows) grid with a spatial resolution of 2.1 km. The environmental forcing factors considered in the present model are sediment-laden river flows and turbidity currents, waves, tides, wind-driven currents, sea level change, submarine slope failure and carbonate sediment production.
DOI: 10.4225/08/52787c877acf6
title: Modelled seabed response to possible climate change scenarios over the next 50 years in the Australian Southeast - High Energy scenario datasets with Sedsim input files and output files

description: Using data from ocean forecast models, field observations and seabed sampling we ran a numerical sediment transport model to estimate the Australian Shelf seabed evolution under three climate change scenarios. This data collection is for the High Energy climate change scenario of:  
    highest rainfall,
    highest sediment load,
    highest outflow, and
    highest oceanographic conditions,
    maximum sea level rise in next 50 years.

In this study, the interaction of seabed sediment types and hydrodynamic forces in the southeastern region has been investigated using a state-of-the-art numerical model, Sedsim. The simulation area  for this collection covers the south-eastern Australian continental shelf and abyssal basins, including Bass Strait, the Tasman Sea, and the Tasmanian coast, as well as part of the South Australian and New South Wales coasts.

The model uses the known grain-size distribution of the present-day seabed based on a comprehensive analysis of currently available seabed data Information available from this data source includes grainsize, mud content, rock exposure, and estimates of critical seabed shear stress. This sediment layer is incorporated in the latest high-resolution (0.0025°) seabed bathymetry obtained from the Australian National Oceans Office (NOO). The seabed topography and present-day sediment layer are represented by a 566 (columns) by 550 (rows) grid with a spatial resolution of 2.1 km. The environmental forcing factors considered in the present model are sediment-laden river flows and turbidity currents, waves, tides, wind-driven currents, sea level change, submarine slope failure and carbonate sediment production.
DOI: 10.4225/08/52787cbe14a06
title: Modelled seabed response to possible climate change scenarios over the next 50 years in the Australian Southeast - Stationary scenario datasets with Sedsim input files and output files

description: Using data from ocean forecast models, field observations and seabed sampling we ran a numerical sediment transport model to estimate the Australian Shelf seabed evolution under three climate change scenarios. This data collection is for the Stationary climate change scenario in which the present climate continues for next 50 years.

In this study, the interaction of seabed sediment types and hydrodynamic forces in the southeastern region has been investigated using a state-of-the-art numerical model, Sedsim. The simulation area  for this collection covers the south-eastern Australian continental shelf and abyssal basins, including Bass Strait, the Tasman Sea, and the Tasmanian coast, as well as part of the South Australian and New South Wales coasts.

The model uses the known grain-size distribution of the present-day seabed based on a comprehensive analysis of currently available seabed data Information available from this data source includes grainsize, mud content, rock exposure, and estimates of critical seabed shear stress. This sediment layer is incorporated in the latest high-resolution (0.0025°) seabed bathymetry obtained from the Australian National Oceans Office (NOO). The seabed topography and present-day sediment layer are represented by a 566 (columns) by 550 (rows) grid with a spatial resolution of 2.1 km. The environmental forcing factors considered in the present model are sediment-laden river flows and turbidity currents, waves, tides, wind-driven currents, sea level change, submarine slope failure and carbonate sediment production.
DOI: 10.4225/08/52787d0f294b5
title: Modelled seabed response to possible climate change scenarios over the next 50 years in the Australian Northeast - Stationary scenario datasets with Sedsim input files and output files

description: Using data from ocean forecast models, field observations and seabed sampling we ran a numerical sediment transport model to estimate the Australian Shelf seabed evolution under three climate change scenarios. This data collection is for the Stationary climate change scenario in which the present climate continues for next 50 years.

In this study, the interaction of seabed sediment types and hydrodynamic forces in the northeastern region has been investigated using a state-of-the-art numerical model, Sedsim. The simulation area  for this collection covers the northeast Australia continental shelf and abyssal basins which include the Great Barrier Reef, the Marion and Queensland plateaus, the Cato, Townsville and Queensland troughs, the New South Wales Shelf and the coast from south of Jervis Bay up to Princess Charlotte Bay in the North.

The model uses the known grain-size distribution of the present-day seabed based on a comprehensive analysis of currently available seabed data Information available from this data source includes grainsize, mud content, rock exposure, and estimates of critical seabed shear stress. This sediment layer is incorporated in the latest high-resolution (0.0025°) seabed bathymetry obtained from the Australian National Oceans Office (NOO). The seabed topography and present-day sediment layer are represented by a 566 (columns) by 550 (rows) grid with a spatial resolution of 2.1 km. The environmental forcing factors considered in the present model are sediment-laden river flows and turbidity currents, waves, tides, wind-driven currents, sea level change, submarine slope failure and carbonate sediment production.
DOI: 10.4225/08/52787d97b32ad
title: Modelled seabed response to possible climate change scenarios over the next 50 years in the Australian North - High Energy scenario datasets with Sedsim input files and output files

description: Using data from ocean forecast models, field observations and seabed sampling we ran a numerical sediment transport model to estimate the Australian Shelf seabed evolution under three climate change scenarios. This data collection is for the High Energy climate change scenario of:  
    highest rainfall,
    highest sediment load,
    highest outflow, and
    highest oceanographic conditions,
    maximum sea level rise in next 50 years.

In this study, the interaction of seabed sediment types and hydrodynamic forces in the northern region has been investigated using a state-of-the-art numerical model, Sedsim. The simulation area  for this collection covers the Gulf of Carpentaria (GOC), the Torres Strait, north-western part of Coral Sea and the eastern part of Arafura Sea.

The model uses the known grain-size distribution of the present-day seabed based on a comprehensive analysis of currently available seabed data Information available from this data source includes grainsize, mud content, rock exposure, and estimates of critical seabed shear stress. This sediment layer is incorporated in the latest high-resolution (0.0025°) seabed bathymetry obtained from the Australian National Oceans Office (NOO). The seabed topography and present-day sediment layer are represented by a 566 (columns) by 550 (rows) grid with a spatial resolution of 2.1 km. The environmental forcing factors considered in the present model are sediment-laden river flows and turbidity currents, waves, tides, wind-driven currents, sea level change, submarine slope failure and carbonate sediment production.
DOI: 10.1285/i22808949a2n1p25
title: Time to Change. The Six Day War and the Origins of Italy�s Pro-Arab Foreign Policy

description: The Six Day War marked a turning point in Italy�s attitude toward the Arab-Israeli conflict. During the crisis the Italian diplomacy tried to mediate in order to prevent an open war but this policy gave rise to harsh polemics among the coalition government. These disagreements revealed a deep rooted change which involved political and security matters. Energy issues became a top priority in the economic and political agenda and most of the Italian public opinion shifted toward a pro-Arab stance while the memories of the Holocaust were fading away. Moreover, the growing Soviet infiltration in the Mediterranean drove the Italian government to envisage security on a global scale while Israel maintained a regional approach. All these differences contributed in gradually shaping a new trend in Israeli-Italian relationships which lasted for a long time.
DOI: 10.1285/i22808949a2n1p7
title: Sobre el proceso soberanista abierto en Catalunya y su Encaje Constitucional

description: This article maintains a concept of democratic constitution that is opposed to the inquisitorial and totalitarian constitution. The supreme norms of the Constitution cannot become an element to prohibit any initiative of a "part" to be converted into a "whole" when the constitutional reform is impossible to be carried out. On the other hand, in the sovereignist catalan process, there is a political conflict and the Constitutional Court becomes an element of the political decision to suspend a parliamentary declaration that considered the Catalan people sovereign political subject, with no legal effect. Confusing politics and law is especially serious because it helps to forget the great responsibility of rulers, which is promising to give intelligent answers to citizenship. In a democratic system, metaphysics cannot be imposed constitutional popular will. The misunderstanding of the "madrile�ismo politico" is dangerous because it exacerbates a latent problem in the history of Spain, which is producing a shock of legitimacy and emotions.
DOI: 10.4225/08/52787dcf67fca
title: Modelled seabed response to possible climate change scenarios over the next 50 years in the Australian North - Low Energy scenario datasets with Sedsim input files and output files

description: Using data from ocean forecast models, field observations and seabed sampling we ran a numerical sediment transport model to estimate the Australian Shelf seabed evolution under three climate change scenarios. This data collection is for the Low Energy climate change scenario of:  
    lowest rainfall,
    lowest sediment load,
    lowest outflow, and
    El-Niño year oceanographic conditions,
    no sea level rise in next 50 years.

In this study, the interaction of seabed sediment types and hydrodynamic forces in the northern region has been investigated using a state-of-the-art numerical model, Sedsim. The simulation area  for this collection covers the Gulf of Carpentaria (GOC), the Torres Strait, north-western part of Coral Sea and the eastern part of Arafura Sea.

The model uses the known grain-size distribution of the present-day seabed based on a comprehensive analysis of currently available seabed data Information available from this data source includes grainsize, mud content, rock exposure, and estimates of critical seabed shear stress. This sediment layer is incorporated in the latest high-resolution (0.0025°) seabed bathymetry obtained from the Australian National Oceans Office (NOO). The seabed topography and present-day sediment layer are represented by a 566 (columns) by 550 (rows) grid with a spatial resolution of 2.1 km. The environmental forcing factors considered in the present model are sediment-laden river flows and turbidity currents, waves, tides, wind-driven currents, sea level change, submarine slope failure and carbonate sediment production.