cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.4195572
title: RPP Kesebangunan dan Kekongruenan - Diny Anggriani A

description: Kesebangunan dan kekongruenan biasanya digunakan untuk membandingkan dua buah bangun datar (atau lebih) dengan bentuk yang sama. dua buah bangun datar dapat dikatakan sebangun apabila panjang setiap sisi pada kedua bangun datar tersebut memiliki nilai perbandingan yang sama. Sedangkan kongruen memiliki konsep yang lebih mendetail, apabila dua buah (atau lebih) bangun datar memiliki bentuk, ukuran, serta besar sudut yang sama barulah mereka dapat disebut sebagai bangun datar yang kongruen.Kesebangunan dan Kekongruenan sebenarnya memiliki konsep yang sederhana. Akan tetapi apabila kita tidak memahaminya dengan baik, terkadang kita terbalik dalam mendefinisikan keduanya.Game tebak ruang ini dirancang agar memudahkan siswa dalam memahami konsep Kesebangunan dan Kekongruenan. Siswa menjadi lebih mudah dalam mengenali bangun – bangun datar yang sebangun atau tidak sebangun dan mengenali bangun datar yang kongruen ataupun tidak kongruen. Dikemas menjadi game yang menarik sehingga siswa menjadi lebih mudah mengerti konsep materi tersebut.<br>
DOI: 10.7910/dvn/v1rjpf/9abngm
title: cbb20160406_03.txt.gz

description: :unav
DOI: 10.6084/m9.figshare.4195572.v1
title: RPP Kesebangunan dan Kekongruenan - Diny Anggriani A

description: Kesebangunan dan kekongruenan biasanya digunakan untuk membandingkan dua buah bangun datar (atau lebih) dengan bentuk yang sama. dua buah bangun datar dapat dikatakan sebangun apabila panjang setiap sisi pada kedua bangun datar tersebut memiliki nilai perbandingan yang sama. Sedangkan kongruen memiliki konsep yang lebih mendetail, apabila dua buah (atau lebih) bangun datar memiliki bentuk, ukuran, serta besar sudut yang sama barulah mereka dapat disebut sebagai bangun datar yang kongruen.Kesebangunan dan Kekongruenan sebenarnya memiliki konsep yang sederhana. Akan tetapi apabila kita tidak memahaminya dengan baik, terkadang kita terbalik dalam mendefinisikan keduanya.Game tebak ruang ini dirancang agar memudahkan siswa dalam memahami konsep Kesebangunan dan Kekongruenan. Siswa menjadi lebih mudah dalam mengenali bangun – bangun datar yang sebangun atau tidak sebangun dan mengenali bangun datar yang kongruen ataupun tidak kongruen. Dikemas menjadi game yang menarik sehingga siswa menjadi lebih mudah mengerti konsep materi tersebut.<br>
DOI: 10.7910/dvn/v1rjpf/k0rezg
title: cbb20160913_03.txt.gz

description: :unav
DOI: 10.6084/m9.figshare.4193589
title: Metadynamics simulation of an IDR region in yeast SAC6 protein

description: In yeast SAC6 protein, between the domains, short sequences of amino acids have no defined secondary structures. By using Metadynamics simulation, we explored the dynamics of this region with T103 phosphorylated or non-phosphorylated.
DOI: 10.7910/dvn/v1rjpf/vbtcub
title: cbb20160628_03.txt.gz

description: :unav
DOI: 10.7910/dvn/v1rjpf/cxv63v
title: cbb20161101_03.txt.gz

description: :unav
DOI: 10.7910/dvn/v1rjpf/fyapyy
title: cbb20160811_03.txt.gz

description: :unav
DOI: 10.7910/dvn/v1rjpf/bhor8f
title: cbb20160218_03.txt.gz

description: :unav
DOI: 10.7910/dvn/v1rjpf/v1murb
title: cbb20161120_03.txt.gz

description: :unav
DOI: 10.6084/m9.figshare.4193589.v3
title: Metadynamics simulation of an IDR region in yeast SAC6 protein

description: In yeast SAC6 protein, between the domains, short sequences of amino acids have no defined secondary structures. By using Metadynamics simulation, we explored the dynamics of this region with T103 phosphorylated or non-phosphorylated.
DOI: 10.6084/m9.figshare.4193589.v5
title: Metadynamics simulation of an IDR region in yeast SAC6 protein

description: In yeast SAC6 protein, between the domains, short sequences of amino acids have no defined secondary structures. By using Metadynamics simulation, we explored the dynamics of this region with T103 phosphorylated or non-phosphorylated.
DOI: 10.7910/dvn/v1rjpf/hrh2x3
title: cbb20160117_03.txt.gz

description: :unav
DOI: 10.6084/m9.figshare.4193589.v4
title: Metadynamics simulation of an IDR region in yeast SAC6 protein

description: In yeast SAC6 protein, between the domains, short sequences of amino acids have no defined secondary structures. By using Metadynamics simulation, we explored the dynamics of this region with T103 phosphorylated or non-phosphorylated.
DOI: 10.7910/dvn/v1rjpf/8zwudp
title: cbb20161015_03.txt.gz

description: :unav
DOI: 10.7910/dvn/v1rjpf/sn4joe
title: cbb20160423_03.txt.gz

description: :unav
DOI: 10.7910/dvn/v1rjpf/assonj
title: cbb20161017_03.txt.gz

description: :unav
DOI: 10.6084/m9.figshare.4193457
title: pyramidalCells_ascFiles.zip

description: Specification in .asc format of the 288 pyramidal cells analyzed in the paper "Wiring economy of pyramidal cells in the juvenile rat somatosensory cortex". The software for analyzing the wiring optimality is freely available at the Computational Intelligence Group's webpage (http://cig.fi.upm.es/ Software section)
DOI: 10.6084/m9.figshare.4193457.v1
title: pyramidalCells_ascFiles.zip

description: Specification in .asc format of the 288 pyramidal cells analyzed in the paper "Wiring economy of pyramidal cells in the juvenile rat somatosensory cortex". The software for analyzing the wiring optimality is freely available at the Computational Intelligence Group's webpage (http://cig.fi.upm.es/ Software section)
DOI: 10.7910/dvn/v1rjpf/zsxqoh
title: cbb20161224_03.txt.gz

description: :unav
DOI: 10.6084/m9.figshare.4192260
title: PONE-D-16-31823R1_dataset

description: This dataset is for the paper numbered PONE-D-16-31823R1.
DOI: 10.7910/dvn/v1rjpf/7its0c
title: cbb20161219_03.txt.gz

description: :unav
DOI: 10.6084/m9.figshare.4192260.v1
title: PONE-D-16-31823R1_dataset

description: This dataset is for the paper numbered PONE-D-16-31823R1.
DOI: 10.6084/m9.figshare.4187295
title: Regionalized Mediterranean SSP population projections

description: You can find spatially explicit population projections for the Mediterranean region for the five Shared Socioeconomic Pathways (SSPs). The raster files are available as GeoTIFF format and have a spatial resolution of 30 arc seconds (~1km at the equator). Data are available in 5-year increments from 2015 to 2100 for each SSP.<br><br>For more information see:<br>Reimann, L, Merkens, J-L, Vafeidis, A T (2018): Regionalized Shared Socioeconomic Pathways: narratives and spatial population projections for the Mediterranean coastal zone. In: Regional Environmental Change 18, 235-245. DOI: 10.1007/s10113-017-1189-2.
DOI: 10.7910/dvn/v1rjpf/pbpfbi
title: cbb20160331_03.txt.gz

description: :unav
DOI: 10.7910/dvn/v1rjpf/ejaui4
title: cbb20160725_03.txt.gz

description: :unav
DOI: 10.6084/m9.figshare.4185096
title: Age and emplacement of the Permian–Jurassic Menghai batholith, Western Yunnan, China

description: The Menghai batholith (Yunnan Province, China) is the southern extension of the ~370 km long Lincang granite body that syntectonically intruded the collisional zone between Gondwana (Baoshan block) and Laurasia (Simao block) terranes during closure of the Palaeo-Tethyan Ocean. Eight Menghai granodiorites were analysed across an ~45 km E–W transect from the pluton’s central region to eastern perimeter. Each rock was imaged in cathodoluminescence and geochemically analysed for major and trace elements. A minimum 30 zircons per sample were dated using laser ablation inductively coupled plasma–mass spectrometry. Samples are peraluminous to strongly peraluminous, magnesian, calcic or calc-alkalic granodiorites. Trace element suggest a high pressure (12–15 kbar) low clay source with &gt;20–30% volume interaction with basalt. Crustal anatexis was likely related to post-collisional lithosphere delamination and upwelling of hot asthenosphere, forming large-volume melts. Zircon ages (<sup>207</sup>Pb–<sup>206</sup>Pb and <sup>238</sup>U–<sup>206</sup>Pb) range from 3234 ± 42 to 171.7 ± 5.4 Ma (±2<i>σ</i>). Inherited zircon ages include the Palaeoarchaean–Neoarchaean (average 2938 ± 27 Ma, <i>n</i> = 8 ages), Lüliang (2254 ± 38 Ma, <i>n</i> = 7), Changcheng–Jixianian (1274 ± 47 Ma, <i>n</i> = 33), Qinbaikou (963 ± 29 Ma, <i>n</i> = 7), Nanhua (787 ± 24 Ma, <i>n</i> = 7), Sinian (595.4 ± 12.2 Ma, <i>n</i> = 14), Qilian (452.2 ± 8.7 Ma, <i>n</i> = 24) and Tienshan (358.9 ± 12.4 Ma, <i>n</i> = 5). The presence of these ages decrease from the batholith’s central portion (&gt;50% ages) to eastern perimeter (2–16% ages), as the rocks appear progressively metamorphosed. The distribution of U/Th ratio suggests inherited zircons are Carboniferous (317.6 ± 5.7 Ma) and older and crystallization ages span the Permian to Early Jurassic. The average and youngest zircon age per sample decreases from the centre of the batholith to its eastern perimeter, from 226.8 ± 8.8 and 210.7 ± 3.3 to 211.8 ± 5.7 and 171.0 ± 5.4 Ma, respectively. If recorded by syntectonic zircon crystallization, collision and closure of a branch of the Palaeo-Tethyan Ocean occurred here over an ~100 million years time period from the Permian (281.0 ± 13.0 Ma) to Jurassic (171.5 ± 5.4 Ma).
DOI: 10.6084/m9.figshare.4185060
title: Impacts of pellet pH on nitrous oxide emission rates from cattle manure compost pellets

description: Previous reports indicated that the emission of nitrous oxide (N<sub>2</sub>O) when manure compost pellets (MCP) were applied to soil was greater than when ordinary manure compost or inorganic fertilizer was applied, but that applying pellets of nitrogen-enriched manure compost, a by-product of deodorizing manure during composting, resulted in N<sub>2</sub>O emission rates less than those from MCPs. To investigate the mechanism by which N<sub>2</sub>O emission rates and cumulative emissions were reduced in nitrogen-enriched manure composts pellets (N+MCP), we studied the impact of pellet pH on N<sub>2</sub>O emission, because pH is different between MCP (pH 8.6) and N+MCP (pH 5.3). In an incubation experiment, the pH of pellets was adjusted to five levels (5.3, 6.0, 7.0, 8.0 and 8.6) with acid or alkaline solutions, and the pellets were incubated without soil in a beaker at 30°C for 90 d (MCP) or 42 d (N+MCP). A large peak in N<sub>2</sub>O emission rate was observed soon after beginning the incubation (within 1–3 d) in the neutral and alkaline treatments for both MCP and N+MCP, and these peaks corresponded to a rise in the pellet nitrite contents. Thus, this N<sub>2</sub>O emission peak might have been generated by the denitrification of nitrite in the pellets. In the acid treatments of MCP, the N<sub>2</sub>O emission was distributed more in the later incubation period (14–90 d), when the reduction of nitrate in MCP occurred. This led to a significant increase in cumulative N<sub>2</sub>O emission as compared with the alkaline treatments for MCP. Regarding the mechanism by which N<sub>2</sub>O emission was reduced in N+MCP, although larger cumulative N<sub>2</sub>O emission rates in the earlier stage (0–14 d for MCP and 0–7 d for N+MCP) were observed when the pellet pH was adjusted close to 7.0, lowering the pH of MCP to 5.3 (the pH of N+MCP) did not demonstrate a significant decrease in cumulative N<sub>2</sub>O emission as compared with the original pH treatment (pH 8.6). These results indicate that pellet pH might not relate directly to the mechanism by which N<sub>2</sub>O emission was reduced in N+MCP.
DOI: 10.7910/dvn/v1rjpf/6xhjks
title: cbb20160309_03.txt.gz

description: :unav
DOI: 10.6084/m9.figshare.4185060.v1
title: Impacts of pellet pH on nitrous oxide emission rates from cattle manure compost pellets

description: Previous reports indicated that the emission of nitrous oxide (N<sub>2</sub>O) when manure compost pellets (MCP) were applied to soil was greater than when ordinary manure compost or inorganic fertilizer was applied, but that applying pellets of nitrogen-enriched manure compost, a by-product of deodorizing manure during composting, resulted in N<sub>2</sub>O emission rates less than those from MCPs. To investigate the mechanism by which N<sub>2</sub>O emission rates and cumulative emissions were reduced in nitrogen-enriched manure composts pellets (N+MCP), we studied the impact of pellet pH on N<sub>2</sub>O emission, because pH is different between MCP (pH 8.6) and N+MCP (pH 5.3). In an incubation experiment, the pH of pellets was adjusted to five levels (5.3, 6.0, 7.0, 8.0 and 8.6) with acid or alkaline solutions, and the pellets were incubated without soil in a beaker at 30°C for 90 d (MCP) or 42 d (N+MCP). A large peak in N<sub>2</sub>O emission rate was observed soon after beginning the incubation (within 1–3 d) in the neutral and alkaline treatments for both MCP and N+MCP, and these peaks corresponded to a rise in the pellet nitrite contents. Thus, this N<sub>2</sub>O emission peak might have been generated by the denitrification of nitrite in the pellets. In the acid treatments of MCP, the N<sub>2</sub>O emission was distributed more in the later incubation period (14–90 d), when the reduction of nitrate in MCP occurred. This led to a significant increase in cumulative N<sub>2</sub>O emission as compared with the alkaline treatments for MCP. Regarding the mechanism by which N<sub>2</sub>O emission was reduced in N+MCP, although larger cumulative N<sub>2</sub>O emission rates in the earlier stage (0–14 d for MCP and 0–7 d for N+MCP) were observed when the pellet pH was adjusted close to 7.0, lowering the pH of MCP to 5.3 (the pH of N+MCP) did not demonstrate a significant decrease in cumulative N<sub>2</sub>O emission as compared with the original pH treatment (pH 8.6). These results indicate that pellet pH might not relate directly to the mechanism by which N<sub>2</sub>O emission was reduced in N+MCP.
DOI: 10.6084/m9.figshare.4185096.v1
title: Age and emplacement of the Permian–Jurassic Menghai batholith, Western Yunnan, China

description: The Menghai batholith (Yunnan Province, China) is the southern extension of the ~370 km long Lincang granite body that syntectonically intruded the collisional zone between Gondwana (Baoshan block) and Laurasia (Simao block) terranes during closure of the Palaeo-Tethyan Ocean. Eight Menghai granodiorites were analysed across an ~45 km E–W transect from the pluton’s central region to eastern perimeter. Each rock was imaged in cathodoluminescence and geochemically analysed for major and trace elements. A minimum 30 zircons per sample were dated using laser ablation inductively coupled plasma–mass spectrometry. Samples are peraluminous to strongly peraluminous, magnesian, calcic or calc-alkalic granodiorites. Trace element suggest a high pressure (12–15 kbar) low clay source with &gt;20–30% volume interaction with basalt. Crustal anatexis was likely related to post-collisional lithosphere delamination and upwelling of hot asthenosphere, forming large-volume melts. Zircon ages (<sup>207</sup>Pb–<sup>206</sup>Pb and <sup>238</sup>U–<sup>206</sup>Pb) range from 3234 ± 42 to 171.7 ± 5.4 Ma (±2<i>σ</i>). Inherited zircon ages include the Palaeoarchaean–Neoarchaean (average 2938 ± 27 Ma, <i>n</i> = 8 ages), Lüliang (2254 ± 38 Ma, <i>n</i> = 7), Changcheng–Jixianian (1274 ± 47 Ma, <i>n</i> = 33), Qinbaikou (963 ± 29 Ma, <i>n</i> = 7), Nanhua (787 ± 24 Ma, <i>n</i> = 7), Sinian (595.4 ± 12.2 Ma, <i>n</i> = 14), Qilian (452.2 ± 8.7 Ma, <i>n</i> = 24) and Tienshan (358.9 ± 12.4 Ma, <i>n</i> = 5). The presence of these ages decrease from the batholith’s central portion (&gt;50% ages) to eastern perimeter (2–16% ages), as the rocks appear progressively metamorphosed. The distribution of U/Th ratio suggests inherited zircons are Carboniferous (317.6 ± 5.7 Ma) and older and crystallization ages span the Permian to Early Jurassic. The average and youngest zircon age per sample decreases from the centre of the batholith to its eastern perimeter, from 226.8 ± 8.8 and 210.7 ± 3.3 to 211.8 ± 5.7 and 171.0 ± 5.4 Ma, respectively. If recorded by syntectonic zircon crystallization, collision and closure of a branch of the Palaeo-Tethyan Ocean occurred here over an ~100 million years time period from the Permian (281.0 ± 13.0 Ma) to Jurassic (171.5 ± 5.4 Ma).
DOI: 10.6084/m9.figshare.4183560
title: Data_Beyond_Synchrony.xlsx

description: The EXCEL file contains the data on which the article "Beyond synchrony: Joint action in a complex production task reveals beneficial effects of decreased interpersonal synchrony", published in Plos One by Sebastian Wallot, Panagiotis Mitkidis, John McGraw and Andreas Roepstorff is based.The EXCEL file contains two sheets: The first sheet (data) contains all data in columns for each observable. The second sheet (legend) contains a legend for the data set, describing each observable.
DOI: 10.6084/m9.figshare.4183560.v1
title: Data_Beyond_Synchrony.xlsx

description: The EXCEL file contains the data on which the article "Beyond synchrony: Joint action in a complex production task reveals beneficial effects of decreased interpersonal synchrony", published in Plos One by Sebastian Wallot, Panagiotis Mitkidis, John McGraw and Andreas Roepstorff is based.The EXCEL file contains two sheets: The first sheet (data) contains all data in columns for each observable. The second sheet (legend) contains a legend for the data set, describing each observable.
DOI: 10.7910/dvn/v1rjpf/oetkoo
title: cbb20161023_03.txt.gz

description: :unav
DOI: 10.6084/m9.figshare.4181883
title: Enhanced torsional actuation and stress coupling in Mn-modified 0.93(Na<sub>0.5</sub>Bi<sub>0.5</sub>TiO<sub>3</sub>)-0.07BaTiO<sub>3</sub> lead-free piezoceramic system

description: This paper is concerned with the development of a piezoelectric <i>d</i><sub>15</sub> shear-induced torsion actuator made of a lead-free piezoceramic material exhibiting giant piezoelectric shear stress coefficient (<i>e</i><sub>15</sub>) and piezoelectric transverse shear actuation force comparable to that of lead-based shear-mode piezoceramics. The Mn-modified 0.93(Na<sub>0.5</sub>Bi<sub>0.5</sub>TiO<sub>3</sub>)-0.07BaTiO<sub>3</sub> (NBT-BT-Mn) composition exhibited excellent properties as a torsional transducer with piezoelectric shear stress coefficient on the order of 11.6 C m<sup>–2</sup>. The torsional transducer, consisting of two oppositely polarized NBT-BT-Mn <i>d</i><sub>15</sub> mode piezoceramic shear patches, provided a rate of twist of 0.08 mm m<sup>–1</sup> V<sup>–1</sup> under quasi-static 150 V drive. The high value of piezoelectric shear <i>d</i><sub>15</sub> coefficient in NBT-BT-Mn sample further demonstrated its potential in practical applications. These results confirm that the lead-free piezoceramics can be as effective as their lead-based counterparts.
DOI: 10.7910/dvn/v1rjpf/o6eqfo
title: cbb20160608_03.txt.gz

description: :unav
DOI: 10.7910/dvn/v1rjpf/s0kotb
title: cbb20160103_03.txt.gz

description: :unav
DOI: 10.6084/m9.figshare.4181883.v2
title: Enhanced torsional actuation and stress coupling in Mn-modified 0.93(Na<sub>0.5</sub>Bi<sub>0.5</sub>TiO<sub>3</sub>)-0.07BaTiO<sub>3</sub> lead-free piezoceramic system

description: This paper is concerned with the development of a piezoelectric <i>d</i><sub>15</sub> shear-induced torsion actuator made of a lead-free piezoceramic material exhibiting giant piezoelectric shear stress coefficient (<i>e</i><sub>15</sub>) and piezoelectric transverse shear actuation force comparable to that of lead-based shear-mode piezoceramics. The Mn-modified 0.93(Na<sub>0.5</sub>Bi<sub>0.5</sub>TiO<sub>3</sub>)-0.07BaTiO<sub>3</sub> (NBT-BT-Mn) composition exhibited excellent properties as a torsional transducer with piezoelectric shear stress coefficient on the order of 11.6 C m<sup>–2</sup>. The torsional transducer, consisting of two oppositely polarized NBT-BT-Mn <i>d</i><sub>15</sub> mode piezoceramic shear patches, provided a rate of twist of 0.08 mm m<sup>–1</sup> V<sup>–1</sup> under quasi-static 150 V drive. The high value of piezoelectric shear <i>d</i><sub>15</sub> coefficient in NBT-BT-Mn sample further demonstrated its potential in practical applications. These results confirm that the lead-free piezoceramics can be as effective as their lead-based counterparts.
DOI: 10.7910/dvn/v1rjpf/betzth
title: cbb20160915_03.txt.gz

description: :unav
DOI: 10.6084/m9.figshare.4181883.v1
title: Enhanced torsional actuation and stress coupling in Mn-modified 0.93(Na<sub>0.5</sub>Bi<sub>0.5</sub>TiO<sub>3</sub>)-0.07BaTiO<sub>3</sub> lead-free piezoceramic system

description: This paper is concerned with the development of a piezoelectric <i>d</i><sub>15</sub> shear-induced torsion actuator made of a lead-free piezoceramic material exhibiting giant piezoelectric shear stress coefficient (<i>e</i><sub>15</sub>) and piezoelectric transverse shear actuation force comparable to that of lead-based shear-mode piezoceramics. The Mn-modified 0.93(Na<sub>0.5</sub>Bi<sub>0.5</sub>TiO<sub>3</sub>)-0.07BaTiO<sub>3</sub> (NBT-BT-Mn) composition exhibited excellent properties as a torsional transducer with piezoelectric shear stress coefficient on the order of 11.6 C m<sup>–2</sup>. The torsional transducer, consisting of two oppositely polarized NBT-BT-Mn <i>d</i><sub>15</sub> mode piezoceramic shear patches, provided a rate of twist of 0.08 mm m<sup>–1</sup> V<sup>–1</sup> under quasi-static 150 V drive. The high value of piezoelectric shear <i>d</i><sub>15</sub> coefficient in NBT-BT-Mn sample further demonstrated its potential in practical applications. These results confirm that the lead-free piezoceramics can be as effective as their lead-based counterparts.
DOI: 10.7910/dvn/v1rjpf/w09g8z
title: cbb20160304_03.txt.gz

description: :unav
DOI: 10.7910/dvn/v1rjpf/mc7i0p
title: cbb20160610_03.txt.gz

description: :unav
DOI: 10.7910/dvn/v1rjpf/n699fv
title: cbb20160719_03.txt.gz

description: :unav
DOI: 10.7910/dvn/v1rjpf/2wewma
title: cbb20160116_03.txt.gz

description: :unav
DOI: 10.6084/m9.figshare.4176462
title: A multidecadal oscillation in the northeastern Pacific

description: The internal modes of the North Pacific can lead to climatic oscillations through ocean–atmosphere interactions and induce global climate responses. The best example is the Pacific Decadal Oscillation, but this fails to explain many climate phenomena. Here, another multidecadal variability over the North Pacific is described, found by analyzing reconstructed data covering the past 140 years. It is named the Pacific Multidecadal Oscillation (PMO), with anomalously high/low SSTs over the northeastern Pacific, and a quasi-60-year cycle. Related to this low-frequency variability of SST, the global mean temperature and precipitation present significant interdecadal differences. More importantly, the PMO index leads the global mean surface air temperature and SST by one to three years. The Arctic Oscillation pattern and atmospheric circulations are shown to change substantially with the transition of the PMO mode from positive to negative phases. This multidecadal oscillation improves the prospect for a long-term forecast of the global warming trend, since the PMO bears a remarkable relationship with global temperature.
DOI: 10.7910/dvn/v1rjpf/bqszpt
title: cbb20160317_03.txt.gz

description: :unav
DOI: 10.7910/dvn/v1rjpf/zhqdta
title: cbb20160303_03.txt.gz

description: :unav