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  • 1
    Publication Date: 2016-09-10
    Description: Scatter plots of Ertel potential vorticity, Q , versus Bernoulli streamfunction, B , on potential-temperature surfaces, θ , are investigated for Mars using the global Mars Analysis Correction Data Assimilation (MACDA) reanalysis, which spans Mars Year (MY) 24.39 to 27.24. In mid-latitudes, Mars exhibits monotonic, function-like Q ( B ) correlations on θ surfaces similar to those observed for Earth. We quantify this with linear regressions of Q versus B over the vertical range θ  = 400 to 900 K (~30 to 60 km). In autumn, winter and spring, in both hemispheres, the nondimensionalized correlation generally lies between zero and unity and gradually decreases with height, whereas in northern summer, it swings negative. These characteristics match Earth's lower mesosphere ( θ  = 2000 to 3000 K; z  ≈ 48 to 62 k m ) during the same seasons. The exception is southern summer, when the correlation on Mars nearly vanishes. In time series, the transition into and out of northern summer is sinuous and centred just after solar longitude L s  = 90 ∘ , whereas in southern summer it is abrupt and spans ΔL s  ≈ 120 ∘ , which is 1/3 of a Mars year. A striking feature seen on Mars but not on Earth is a large range of Q over the narrow domain of B poleward of each winter polar jet, particularly in the north, which is consistent with the known annular structure of the Martian polar vortex. Froude number calculations suggest the existence of a planetary-scale hydraulic jump associated with the winter polar jet.
    Print ISSN: 0035-9009
    Electronic ISSN: 1477-870X
    Topics: Geography , Physics
    Published by Wiley
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  • 2
    Publication Date: 2015-03-26
    Description: We investigate the correlation of Ertel potential vorticity, Q , with Bernoulli streamfunction, B , on potential-temperature surfaces, θ , in Earth's atmosphere poleward of ±30° latitude. For input we use the 1979–2010 CMAM30-SD specified-dynamics data set. We fit the model Q = Q exp[− λ 0 ( B − B 0 )] separately in the midlatitude [30°,60°) and polar [60°,90°] regions, and nondimensionalize the slope parameter as . In the troposphere, the peak of is approximately 2–3 in winter and 3–4 in summer in both regions. In the stratosphere during winter, both and hover around unity. In spring and fall, continues to hover near unity, but rises by a factor of two, with its maximum located at θ ∼ 700 to 900 K. In summer the polar value drops to , while the midlatitude value swings negative to to −3. In the mesosphere, exhibits incessant fluctuations with values that usually fall within the range 0 to 1. The results support the paradigm for dynamically active regions primarily in the vicinity of θ ∼ 3000–4000K (∼62–72 km) in the mesosphere, whereas except in summer, we get the simple result that the monthly climate-averaged profile, , in the polar regions is nearly unity across the entire stratosphere. During extended recoveries following SSWs, the midlatitude vertical profile develops a peak near 2000 K that descends over the course of a few weeks, alongside the descent of the elevated stratopause in the polar region. This article is protected by copyright. All rights reserved.
    Electronic ISSN: 1942-2466
    Topics: Geography , Geosciences
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 3
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    American Association for the Advancement of Science (AAAS)
    Publication Date: 2000-09-08
    Description: Large-scale nonlinear simulations of Jupiter's 5-micron hot spots produce long-lived coherent structures that cause subsidence in local regions, explaining the low cloudiness and the dryness measured by the Galileo probe inside a hot spot. Like observed hot spots, the simulated coherent structures are equatorially confined, have periodic spacing, propagate west relative to the flow, are generally confined to one hemisphere, and have an anticyclonic gyre on their equatorward side. The southern edge of the simulated hot spots develops vertical shear of up to 70 meters per second in the eastward wind, which can explain the results of the Galileo probe Doppler wind experiment.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Showman, A P -- Dowling, T E -- New York, N.Y. -- Science. 2000 Sep 8;289(5485):1737-40.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉National Research Council (NRC)/NASA Ames Research Center, Mail Stop 245-3, Moffett Field, CA 94035-1000, USA. showman@humbabe.arc.nasa.gov〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/10976064" target="_blank"〉PubMed〈/a〉
    Keywords: *Ammonia ; Extraterrestrial Environment ; *Hydrogen Sulfide ; *Jupiter ; Pressure ; Temperature ; *Water
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 4
    Publication Date: 2008-05-10
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Dowling, Timothy E -- England -- Nature. 2008 May 8;453(7192):163-4. doi: 10.1038/453163a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18464726" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 5
    Publication Date: 1995-03-03
    Description: Hubble Space Telescope (HST) images reveal major atmospheric changes created by the collision of comet Shoemaker-Levy 9 with Jupiter. Plumes rose to 3000 kilometers with ejection velocities on the order of 10 kilometers second-1; some plumes were visible in the shadow of Jupiter before rising into sunlight. During some impacts, the incoming bolide may have been detected. Impact times were on average about 8 minutes later than predicted. Atmospheric waves were seen with a wave front speed of 454 +/- 20 meters second-1. The HST images reveal impact site evolution and record the overall change in Jupiter's appearance as a result of the bombardment.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Hammel, H B -- Beebe, R F -- Ingersoll, A P -- Orton, G S -- Mills, J R -- Simon, A A -- Chodas, P -- Clarke, J T -- De Jong, E -- Dowling, T E -- New York, N.Y. -- Science. 1995 Mar 3;267(5202):1288-96.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge 02139.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/7871425" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere ; *Extraterrestrial Environment ; *Jupiter ; *Solar System
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 6
    Publication Date: 2012-04-21
    Description: The horizontal pressure-gradient force is traditionally discretized in partial-differential equation (PDE) form in atmospheric models, but may alternatively be discretized as the net normal surface force divided by the mass, which is referred to as the Green–Gauss method in computational fluid dynamics (CFD). The latter approach is ubiquitous in engineering because of the utility of unstructured grids; in the meteorological context Lin derived in 1997 a two-dimensional (2D), plane-parallel, Green–Gauss algorithm and showed that it eliminated inaccuracies related to using terrain-following (sigma) coordinates in steep terrain. Although a hierarchy of three-dimensional (3D) algorithms have been developed by the CFD community, with varying cost-to-benefit trade-offs, work remains to be done to take full advantage of the 3D approach in atmospheric models. Here, we move in this direction by extending Lin's 2D algorithm to 3D. As is true of all Green–Gauss implementations, our algorithm is the same regardless of choice of vertical coordinate or number of fluid constituents. We show that the modifications to the 2D algorithm may be written in the form of additive terms composed of differences of the squares of the top and bottom tilts of the finite-volume faces; the cases for which the 2D and 3D algorithms are identical are then straightforward to discern. For plane-parallel geometry, we include explicit finite-volume formulae for the longitude–latitude and general convex quadrilateral planforms, which includes the cubed-sphere grid, with arbitrary geopotentials on the eight corners. Compared with the 2D version, the 3D algorithm yields approximately a 10% reduction in truncation error and, in the context of a general circulation model, it requires only about a 1% increase in run time. Copyright © 2012 Royal Meteorological Society
    Print ISSN: 0035-9009
    Electronic ISSN: 1477-870X
    Topics: Geography , Physics
    Published by Wiley
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  • 7
    Publication Date: 1986-07-04
    Description: Voyager 2 images of the southern hemisphere of Uranus indicate that submicrometersize haze particles and particles of a methane condensation cloud produce faint patterns in the atmosphere. The alignment of the cloud bands is similar to that of bands on Jupiter and Saturn, but the zonal winds are nearly opposite. At mid-latitudes (-70 degrees to -27 degrees ), where winds were measured, the atmosphere rotates faster than the magnetic field; however, the rotation rate of the atmosphere decreases toward the equator, so that the two probably corotate at about -20 degrees . Voyager images confirm the extremely low albedo of the ring particles. High phase angle images reveal on the order of 10(2) new ringlike features of very low optical depth and relatively high dust abundance interspersed within the main rings, as well as a broad, diffuse, low optical depth ring just inside the main rings system. Nine of the newly discovered small satellites (40 to 165 kilometers in diameter) orbit between the rings and Miranda; the tenth is within the ring system. Two of these small objects may gravitationally confine the e ring. Oberon and Umbriel have heavily cratered surfaces resembling the ancient cratered highlands of Earth's moon, although Umbriel is almost completely covered with uniform dark material, which perhaps indicates some ongoing process. Titania and Ariel show crater populations different from those on Oberon and Umbriel; these were probably generated by collisions with debris confined to their orbits. Titania and Ariel also show many extensional fault systems; Ariel shows strong evidence for the presence of extrusive material. About halfof Miranda's surface is relatively bland, old, cratered terrain. The remainder comprises three large regions of younger terrain, each rectangular to ovoid in plan, that display complex sets of parallel and intersecting scarps and ridges as well as numerous outcrops of bright and dark materials, perhaps suggesting some exotic composition.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Smith, B A -- Soderblom, L A -- Beebe, R -- Bliss, D -- Boyce, J M -- Brahic, A -- Briggs, G A -- Brown, R H -- Collins, S A -- Cook, A F 2nd -- Croft, S K -- Cuzzi, J N -- Danielson, G E -- Davies, M E -- Dowling, T E -- Godfrey, D -- Hansen, C J -- Harris, C -- Hunt, G E -- Ingersoll, A P -- Johnson, T V -- Krauss, R J -- Masursky, H -- Morrison, D -- Owen, T -- Plescia, J B -- Pollack, J B -- Porco, C C -- Rages, K -- Sagan, C -- Shoemaker, E M -- Sromovsky, L A -- Stoker, C -- Strom, R G -- Suomi, V E -- Synnott, S P -- Terrile, R J -- Thomas, P -- Thompson, W R -- Veverka, J -- New York, N.Y. -- Science. 1986 Jul 4;233(4759):43-64.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/17812889" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 8
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Annals of the New York Academy of Sciences 617 (1990), S. 0 
    ISSN: 1749-6632
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Natural Sciences in General
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Journal of fish biology 60 (2002), S. 0 
    ISSN: 1095-8649
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: Squalius alburnoides is a complex of minnows common to the Iberian Peninsula, consisting of two distinct forms. The most common form is comprised of diploid and polyploid asexual hybrids heterozygous for several diagnostic allozyme loci contributed by Squalius pyrenaicus or Squalius carolitertii and a missing ancestor. The other form is diploid and homozygous for the allele contributed by the missing ancestor at these same loci. Present results from analyses of sex ratio and cytochrome b sequences are not consistent with the evolutionary distinctiveness of this non-hybrid form and suggest that it represents an all-male lineage imbedded within an almost all-female complex. This all-male lineage allowed preservation of the ancestral paternal nuclear genome after the paternal ancestor became extinct in all or most drainages, withimportant evolutionary implications.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Journal of fish biology 61 (2002), S. 0 
    ISSN: 1095-8649
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: Neighbour-joining and parsimony analyses identified five lineages of cyprinids: (1) European leuciscins (including Notemigonus)+North American phoxinins (including Phoxinus phoxinus); (2) European gobionins+Pseudorasbora; (3) primarily Asian groups [cultrins+acheilognathins+ gobionins (excluding Abbotina)+xenocyprinins]; (4) Abbottina+Sinocyclocheilus+Acrossocheilus; (5) cyprinins [excluding Sinocyclocheilus and Acrossocheilus]+barbins+labeonins. Relationships among these lineages and the enigmatic taxa Rhodeus were not well-resolved. Tests of monophyly of subfamilies and previously proposed relationships were examined by constraining cytochrome b sequences data to fit previous hypotheses. The analysis of constrained trees indicated that sequence data were not consistent with most previously proposed relationships. Inconsistency was largely attributable to Asian taxa, such as Xenocypris and Xenocyprioides. Improved understanding of historical and taxonomic relationships in Cyprinidae will require further morphological and molecular studies on Asian cyprinids and taxa representative of the diversity found in Africa.
    Type of Medium: Electronic Resource
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