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  • 1
    Publication Date: 2019-07-13
    Description: The role of rotation in planetary atmospheres plays an important role in regulating atmospheric and oceanic heat flow, cloud formation and precipitation. Using the Goddard Institute for Space Studies (GISS) three dimension General Circulation Model (3D-GCM) we demonstrate how varying rotation rate and increasing the incident solar flux on a planet are related to each other and may allow the inner edge of the habitable zone to be much closer than many previous habitable zone studies have indicated. This is shown in particular for fully coupled ocean runs -- some of the first that have been utilized in this context. Results with a 100m mixed layer depth and our fully coupled ocean runs are compared with those of Yang et al. 2014, which demonstrates consistency across models. However, there are clear differences for rotations rates of 1-16x present earth day lengths between the mixed layer and fully couple ocean models, which points to the necessity of using fully coupled oceans whenever possible. The latter was recently demonstrated quite clearly by Hu & Yang 2014 in their aquaworld study with a fully coupled ocean when compared with similar mixed layer ocean studies and by Cullum et al. 2014. Atmospheric constituent amounts were also varied alongside adjustments to cloud parameterizations (results not shown here). While the latter have an effect on what a planet's global mean temperature is once the oceans reach equilibrium they do not qualitatively change the overall relationship between the globally averaged surface temperature and incident solar flux for rotation rates ranging from 1 to 256 times the present Earth day length. At the same time this study demonstrates that given the lack of knowledge about the atmospheric constituents and clouds on exoplanets there is still a large uncertainty as to where a planet will sit in a given star's habitable zone.
    Keywords: Lunar and Planetary Science and Exploration
    Type: GSFC-E-DAA-TN27803 , Comparative Climatology of Terrestrial Planets II: Understanding How Climate Systems Work; Sep 08, 2015 - Sep 11, 2015; Moffet Field, CA; United States
    Format: application/pdf
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  • 2
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Journal of Insect Physiology 4 (1960), S. 92-101 
    ISSN: 0022-1910
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Biology
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1420-9098
    Keywords: Key words: Linepithema humile, vegetation, soil conditions, competition, Portugal.
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary: The overall distribution of Linepithema humile, introduced about a hundred years ago and now widespread in western and southern Portugal, has not notably changed in the last forty years. The ant is particularly common in sand and in clay loam soils but, inexplicably and despite otherwise favourable conditions, is largely absent in adjoining easterly mostly sandy loam soils associated with metamorphic rocks. In these circumstances there was a striking change in transition areas from exclusive dominance by L. humile to exclusive dominance by the competing native species, Crematogaster scutellaris and Pheidole pallidula, which was directly associated with the change in soil type. In a site with a particular sandy loam soil type (Vt) comprising adjoining patches colonized either by L. humile or native ants, the former occurred where there was a greater sand content. In oak planted sandy and Vt soils L. humile was present in cultivated or grazed ground but was replaced by C. scutellaris when there was well established scrub and ground vegetation. There was intense fighting at a transition line in one place with uniform tree and ground vegetation that supported large populations of L. humile and of native dominants on opposite sides of the transition. Here, the former had spread about 30 m per year between 1993 and 1996 compared with an estimated 800 m per year in the first 60 years after introduction. It is concluded that the dominant native C. scutellaris and P. pallidula in their favoured plantation habitats, and T. nigerrimum and T. hispanicum in some arable and pasture habitats can delay or prevent spread of L. humile in soils and vegetation conditions that also suit it. Although L. humile was present in most valley floors, its presence and abundance were not significantly related to valley conditions, and it was sometimes abundant at the tops of adjoining hillsides and in seasonally water-deficient sandy areas. Its association with some built-up areas was strikingly displayed by abundance in a town on inimical metamorphic-based soils that were uncolonized in immediately adjoining vegetationally favourable plantation and agricultural land. The direct and indirect effects of soil type on L. humile are analysed and discussed. Three habitats largely free of human interference – sand dunes with native trees and bare areas, a similarly patchily vegetated rocky river gorge and an eroded arête – may exemplify natural conditions exploited by L. humile in its native South America.
    Type of Medium: Electronic Resource
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