7 research outputs found

    Extent and Causes of Chesapeake Bay Warming

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    Coastal environments such as the Chesapeake Bay have long been impacted by eutrophication stressors resulting from human activities, and these impacts are now being compounded by global warming trends. However, there are few studies documenting long-term estuarine temperature change and the relative contributions of rivers, the atmosphere, and the ocean. In this study, Chesapeake Bay warming, since 1985, is quantified using a combination of cruise observations and model outputs, and the relative contributions to that warming are estimated via numerical sensitivity experiments with a watershed–estuarine modeling system. Throughout the Bay’s main stem, similar warming rates are found at the surface and bottom between the late 1980s and late 2010s (0.02 +/- 0.02C/year, mean +/- 1 standard error), with elevated summer rates (0.04 +/- 0.01C/year) and lower rates of winter warming (0.01 +/- 0.01C/year). Most (~85%) of this estuarine warming is driven by atmospheric effects. The secondary influence of ocean warming increases with proximity to the Bay mouth, where it accounts for more than half of summer warming in bottom waters. Sea level rise has slightly reduced summer warming, and the influence of riverine warming has been limited to the heads of tidal tributaries. Future rates of warming in Chesapeake Bay will depend not only on global atmospheric trends, but also on regional circulation patterns in mid-Atlantic waters, which are currently warming faster than the atmosphere. Supporting model data available at: https://doi.org/10.25773/c774-a36

    Crescimento de Aegla itacolomiensis (Crustacea, Decapoda) em um arroio da Mata AtlĂąntica no sul do Brasil The growth of Aegla itacolomiensis (Crustacea, Decapoda) in an Atlantic forest stream in southern Brazil

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    Analisou-se o crescimento de Aegla itacolomiensis Bond-Buckup & Buckup, 1994, em ambiente natural, a partir de amostragens mensais, realizadas entre junho de 2005 e maio de 2006, no arroio SolitĂĄria Alta, tributĂĄrio da bacia hidrogrĂĄfica do Rio dos Sinos, municĂ­pio de Igrejinha, RS, Brasil (29Âș33'10,2''S; 50Âș50'57''W). Os indivĂ­duos foram coletados com o auxĂ­lio de um puçå, triados por sexo, medidos quanto ao comprimento do cefalotĂłrax (CC) e devolvidos ao arroio no mesmo local de onde foram retirados. O crescimento em comprimento de machos e fĂȘmeas de A. itacolomiensis foi avaliado pela anĂĄlise das distribuiçÔes de frequĂȘncias absolutas em intervalos de classe do CC. As modas dos histogramas de frequĂȘncias do CC foram verificadas. O crescimento dos indivĂ­duos foi estimado por meio da anĂĄlise da progressĂŁo das modas calculadas, resultando nas curvas de crescimento para machos e fĂȘmeas, respectivamente Ct= 23,21[1-e-0,0094 (t + 7,03)] e Ct respectivamente: Ct = 19,49 [1-e-0,0065 (t + 11,16)]. O recrutamento ocorreu na primavera e no verĂŁo. Os machos atingiram tamanhos maiores do que as fĂȘmeas e apresentaram maior taxa de crescimento que estas. A longevidade estimada para os machos foi de 2,2 anos enquanto que para as fĂȘmeas foi de 2,5 anos. O padrĂŁo de crescimento de A. itacolomiensis Ă© semelhante ao de outras espĂ©cies de eglĂ­deos anteriormente estudados.<br>To give more information about ecology and biology of Aegla itacolomiensis Bond-Buckup & Buckup, 1994 was analized its growth in the nature. Monthly samples were made from June 2005 to May 2006 in SolitĂĄria Alta stream, tributary of Rio dos Sinos basin, district of Igrejinha, RS, Brazil (29Âș33'10,2''S; 50Âș50'57''W). The specimens were collected by dip net, sexed and after the cephalotorax measured, the animals were brought back to the stream. The growth estimated by cephalotorax length for males and females of A.itacolomiensis was analized by absolut distributional size-classes frequency. The modal frequency of cephalotorax lenght was calculated. The growth was estimated trought the modal progression. The growth curves in cefalotorax length for males and females are described respectively by the equations: Ct = 23.21[1-e-0.0094 (t + 7.03)] e Ct= 19.49 [1-e-0.0065 (t + 11.16)]. Were found juveniles in the spring and summer. The males attained larger sizes and a higher growth rate than females. The estimated longevity was 2.2 years for males and 2.5 years for females
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