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  • 1
    Publication Date: 2022-05-25
    Description: Author Posting. © Inter-Research, 2013. This article is posted here by permission of Inter-Research for personal use, not for redistribution. The definitive version was published in Marine Ecology Progress Series 484 (2013): 115-130, doi:10.3354/meps10281.
    Description: Environmental temperature and an organism’s ability to respond to it are critical determinants of the geographic distribution of species. Nematostella vectensis is a burrowing sea anemone that inhabits estuaries along the Atlantic coast of North America from Nova Scotia (45°N) to Georgia (31°N). Like other estuarine species, N. vectensis is exposed to large daily (〉20°C) and seasonal (〉25°C) fluctuations in temperature, requiring wide temperature tolerances. At the same time, the natural distribution of this species spans a pronounced thermal cline, which may promote the evolution of different temperature optima and tolerances in populations. We tested the thermal tolerance of N. vectensis adult and developmental stages, which showed all life cycle stages had critical temperatures within 1°C (lethal temperature 39.5 to 40.5°C). When temperature tolerance values were compared with recorded field data, N. vectensis is living in environments very close to their physiological limit. We utilized common garden experiments (13, 21, and 29°C) to test for temperature-specific growth and regeneration rates in N. vectensis from different portions of this species’ range. Temperature had a significant effect on growth and regeneration rate in all clonal lines, with a significant negative relationship between latitude of origin and growth rate at 29°C. Individuals from higher latitudes did not exhibit higher growth rates at cooler temperatures. Together, our results show a combination of broad thermal tolerances for developmental and adult stages and evidence for local adaptation to higher temperatures in populations living in lower latitude locations that would be physiologically compromised with future warming.
    Description: T.C. and S.E. were both supported by the Undergraduate Research Opportunities Program (UROP) at Boston University. A.M.R. was supported by EPA STAR Fellowship F5E11155 to A.M.R. and J.R.F. and the Beacon Institute for Rivers and Estuaries to A.M.R. A.M.T. was supported by MCB-1057354 from the National Science Foundation.
    Keywords: Growth rate ; Latitude ; Local adaptation ; Nematostella ; Regeneration ; Temperature tolerance
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 2
    Publication Date: 2013-08-15
    Description: [1]  This study presents the first report of planetary wave (PW) influences on significant temperature perturbations (10 − 20 K) within a course of one day detected by an Fe lidar from 35 − 51 km in the austral winter of 2011 at McMurdo (77.8°S, 166.7°E), Antarctica. Such large temperature perturbations are captured in the Modern Era Retrospective-Analysis for Research and Applications (MERRA) data, and correspond to various phases of eastward-propagating PWs with periods of 1 − 5 days as revealed in MERRA. The strongest PW dominating the temperature perturbations has a period of 4 − 5 days with wavenumber -1. A 2-day wave with wavenumber -2 and a 1.25-day wave with wavenumber -3 also have significant influences. We find that these eastward propagating PWs are highly confined to winter high latitudes, likely because negative refractive indices equatorward of ~45°S result in evanescent wave characteristics and prevent the PWs from propagating to lower latitudes. The EP flux divergence and instability analyses suggest that barotropic/baroclinic instability at 50 − 60°S induced by the stratospheric polar night jet and/or the “double-jet” structure is the most likely wave source. Such instability in the region poleward of 70°S is a complementary source for the 4-day wave, where we find that the heat flux of the 4-day wave is large and transported from ~70°S toward the pole above 40 km. This transport direction is likely linked to the meridional gradient of background temperature. The migrating diurnal tide near 78°S in the upper stratosphere is discernable, but significantly smaller than that of the dominant 4-day wave.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
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  • 3
    Publication Date: 2014-02-25
    Description: [1]  We provide the first characterization of diurnal and semidiurnal thermal tides in temperature from 30 to 110 km in the winter season (May through August) at McMurdo (77.8°S, 166.7°E), Antarctica. The observations were made with an Fe Boltzmann temperature lidar in 2011 and 2012. Over 330 h of winter data are compiled into a composite day of temperature perturbations that significantly reduce the incoherent wave effects while preserving the coherent tidal signatures. Both diurnal and semidiurnal tides have small amplitudes (less than 3 K) below 100 km with vertical wavelengths of ~29 and ~23 km, respectively. A new finding of this study is the fast growth of diurnal and semidiurnal tidal amplitudes above 100 km to at least 15 K near 110 km, exceeding that of the freely propagating tides originating from the lower atmosphere. Such fast growth exists for all Kp index cases and diurnal amplitude increases to 15 − 30 K at 110 km with larger Kp indices corresponding to larger tidal amplitudes and faster growth rates. The slopes of diurnal tidal phases become steeper above 100 km and the tidal phases barely change with altitude from 100 to 106 km. The tidal growth behavior is reproduced in the Whole Atmosphere Model (WAM) with phases comparable to the observations but magnitudes significantly underestimated. WAM compares reasonably well with the observations below 100 km. The observed significant amplitude increases and phase structure changes suggest additional tidal sources near or above 100 km, which deserve future investigation.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
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