matplotlib/matplotlib v3.1.3

Caswell, Thomas A; Droettboom, Michael; Lee, Antony; Hunter, John; Firing, Eric; Stansby, David; Klymak, Jody M.; Hoffmann, Tim; Andrade, Elliott Sales de; Varoquaux, Nelle; Nielsen, Jens Hedegaard; Root, Benjamin; Elson, Phil; May, Ryan; Dale, Darren; Lee, Jae‐Joon; Seppänen, Janne; McDougall, Damon; Straw, Andrew; Hobson, Paul; Gohlke, Christoph; Yu, Tony S; Ma, Eric; Vincent, Adrien F.; Silvester, Steven; Moad, Charlie; Kniazev, Nikita; Ivanov, Paul; Ernest, Elan; Katins, Jan

doi:10.5281/zenodo.3633844

Cited by 14 publications

(5 citation statements)

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“…aeronomie.be/index.php/data, Thomas et al, 2021;Vandaele et al, 2019), and at NASA's ExoMars archive (https://psg.gsfc.nasa.gov/apps/exomars.php). Figures were made with Matplotlib version 3.2.1 (Caswell et al, 2020), available under the Matplotlib license at https://matplotlib.org/.…”

Section: Conflict Of Interestmentioning

confidence: 99%

The Deuterium Isotopic Ratio of Water Released From the Martian Caps as Measured With TGO/NOMAD

Villanueva

Liuzzi

Aoki

et al. 2022

Geophysical Research Letters

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The evolution and history of water on Mars plays a key role in the assessment of the habitability of the planet across time. There is abundant geomorphological evidence suggesting that Mars had a wetter past (Bibring et al., 2006;Carr & Head, 2003), yet the duration and extent of this more humid past remains a topic of substantial debate. For instance, the large deltas, basins, and valleys on Mars are suggestive of large bodies of water that were stable over relatively long periods of time. Some estimates suggest past volumes of water in excess of a 500 m deep Global Equivalent Layer (GEL; Carr & Head, 2003), which is many times larger than the current estimates of labile water on Mars (∼30 m, Lasue et al., 2013).The large enrichments of D/H measured in atmospheric water suggest that a large fraction, beyond 80%, of this water was lost over time (Jakosky, 2021;Villanueva et al., 2015), and Ar and O isotopic ratios measured with MAVEN (Jakosky et al., 2017) and TGO (Alday, Wilson, et al., 2021) indicate that Mars has lost a large fraction of its atmosphere. Because Mars is less massive than Earth, the neutral escape of volatiles is easier on Mars, considering the similar equilibrium temperatures of the two planets, although Mars is obviously colder. Recent results indicate that most of this escape occurred via neutral and nonionized processes (Brain et al., 2015), in which temperature and its variability across geological times were key factors defining the state of the Martian atmosphere. Recent results from dust storms suggest that dust storms can greatly heat the atmosphere, leading to the upward transport and more readily escape of water (

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Section: Conflict Of Interestmentioning

confidence: 99%

The Deuterium Isotopic Ratio of Water Released From the Martian Caps as Measured With TGO/NOMAD

Villanueva

Liuzzi

Aoki

et al. 2022

Geophysical Research Letters

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“…by the Ministry of Education, Culture, Sports, Science, and Technology (https://search.diasjp.net/ja/dataset/ JRA55). Figures were made with Matplotlib version 3.1.3 (Caswell et al, 2020;Hunter, 2007), available under the Matplotlib license at https://matplotlib.org/. The SOMs analysis is based on the Python package "somoclu" (Wittek et al, 2017).…”

Section: Summary and Discussionmentioning

confidence: 99%

Localized Strong Warming and Humidification Over Winter Japan Tied to Sea Ice Retreat

Tamura

Sato

2023

Geophysical Research Letters

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East Asian winter weather has altered dramatically in response to progressing climate change. However, analysis of time‐averaged atmospheric fields might obscure climate change signals that could relate to specific types of events. This study aimed to detect climate change signals for various background atmospheric fields by applying classification to daily surface pressure patterns. We found a pronounced trend of increase in surface air temperature over Japan since the 1980s, stronger than the seasonal mean trend, when dominating cold air advection from the Sea of Okhotsk. This cold air was warmed and humidified by the retreat of sea ice in the Sea of Okhotsk. In contrast, the warming trend was mitigated when warm air advection was dominant. These results highlight the importance of daily background atmospheric conditions in amplifying and localizing the impact of regional climate change.

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“…DEGs commonly detected by edgeR, DESeq and NOISeq were combined to increase the accuracy of results, and only the genes detected as differentially expressed by all the three tools were used in downstream analyses. To visualize the resulting expression profiles, volcano plots, heatmaps, barplots, and Venn diagrams were prepared for each combination, using stats and graphics core R packages and Python’s Matplotlib 3.2.1 library [ 95 ].…”

Section: Methodsmentioning

confidence: 99%

Salt Stress Tolerance in Casuarina glauca: Insights from the Branchlets Transcriptome

Fernandes

Paulo

Marques

et al. 2022

Plants

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Climate change and the accelerated rate of population growth are imposing a progressive degradation of natural ecosystems worldwide. In this context, the use of pioneer trees represents a powerful approach to reverse the situation. Among others, N2-fixing actinorhizal trees constitute important elements of plant communities and have been successfully used in land reclamation at a global scale. In this study, we have analyzed the transcriptome of the photosynthetic organs of Casuarina glauca (branchlets) to unravel the molecular mechanisms underlying salt stress tolerance. For that, C. glauca plants supplied either with chemical nitrogen (KNO3+) or nodulated by Frankia (NOD+) were exposed to a gradient of salt concentrations (200, 400, and 600 mM NaCl) and RNA-Seq was performed. An average of ca. 25 million clean reads was obtained for each group of plants, corresponding to 86,202 unigenes. The patterns of differentially expressed genes (DEGs) clearly separate two groups: (i) control- and 200 mM NaCl-treated plants, and (ii) 400 and 600 mM NaCl-treated plants. Additionally, although the number of total transcripts was relatively high in both plant groups, the percentage of significant DEGs was very low, ranging from 6 (200 mM NaCl/NOD+) to 314 (600 mM NaCl/KNO3+), mostly involving down-regulation. The vast majority of up-regulated genes was related to regulatory processes, reinforcing the hypothesis that some ecotypes of C. glauca have a strong stress-responsive system with an extensive set of constitutive defense mechanisms, complemented by a tight mechanism of transcriptional and post-transcriptional regulation. The results suggest that the robustness of the stress response system in C. glauca is regulated by a limited number of genes that tightly regulate detoxification and protein/enzyme stability, highlighting the complexity of the molecular interactions leading to salinity tolerance in this species.

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matplotlib/matplotlib v3.1.3

Cited by 14 publications

References 0 publications

The Deuterium Isotopic Ratio of Water Released From the Martian Caps as Measured With TGO/NOMAD

The Deuterium Isotopic Ratio of Water Released From the Martian Caps as Measured With TGO/NOMAD

Localized Strong Warming and Humidification Over Winter Japan Tied to Sea Ice Retreat

Salt Stress Tolerance in Casuarina glauca: Insights from the Branchlets Transcriptome

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