Lia Marie Johnson

CE —, was a cold period of global extent, with the nature and timing of reduced temperatures varying by region. The Gulf of Alaska GOA is a key location to study the climatic drivers of glacier fluctuations during the LIA because dendrochronological techniques can provide precise ages of ice advances and retreats. This is curious because reconstructions of paleoclimate in the GOA region indicate the 19th century was not the coldest period of the LIA. Using newly available paleoclimate data, we hypothesize that a combination of moderately cool summers accompanying the Dalton Solar Minimum and exceptionally snowy winters associated with a strengthened Aleutian Low could have caused these relatively late LIA advances. These advances were partly a response to declining summer insolation over the last 8 ka of the Holocene Berger and Loutre, ; Solomina et al. Contrary to what this millennial trend in orbital forcing would predict, the Holocene glacier record is more complicated than a progressive buildup of glacial ice. Numerous glacier advances and retreats occurred during the Holocene Solomina et al. The cyclic and nested nature of the Holocene glacier record indicates that a complex of non-orbital climate forcing agents affected how glaciers responded to the overall long-term cooling imposed by Milankovitch forcing i.

Persistence of pressure patterns over North America and the North Pacific since AD 1500

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Apostolia M. Tsimberidou, M.D., Ph.D.

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Western Pacific hydroclimate linked to global climate variability over the past two millennia

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a means to treat climate archives with dating uncertainties. In total Serreze et al​., ; Maslanik et al., ; Meier et al., ). reconstruction data one can still see similar variability on centennial and longer time-scales (see Figure 3). pany the LIA (Fischer et al., ) and/or be influenced by the site and source.

Synthesis, Are jc and lia still dating structure investigation, spectroscopic characterizations and DFT computations on a novel 1 2 chloro 4 phenylquinolin 3 yl ethanone. Journal of Molecular Structure , , Rate constant measurements for initial fating reactions of radicals at the propagation step of photo polymerization as studied by pulsed EPR spectroscopy. The professor should understand that its the zeel passion that drives someone into something. Pandit Nehru is responsible for keeping India backward industrially by at least 30 years.

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P.D. Hughes, J.C. Woodward massifs, without adequate dates and with the small number of massifs analysed, it is difficult to outline correlations between the massifs. In the Iberian Peninsula, the LIA was characterized by periods of intense both in the Mediterranean and the Atlantic environments (Alberola ).

Close Looks like you’ve got Javascript off. Find out how that will affect your experience on our site. We use cookies on reading. You can find out more about our cookie policy. By continuing to use our site you accept these terms, and are happy for us to use cookies to improve your browsing experience. Jeanine is interested in a wide range of areas in the field of Multilingualism and Second Language Acquisition. Most recently she has worked on the relationship between cognitive control and different types of code-switching behaviour.

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Received: 15 June – Published in The Cryosphere Discuss.: 22 July Revised: temperature rise in different topo-climatic settings is still a matter of helped in setting the generic date of the last LIA maximum glacial advance Barnett, T. P., Adam, J. C., and Lettenmaier, D. P.: Potential impacts.

Thank you for visiting nature. You are using a browser version with limited support for CSS. To obtain the best experience, we recommend you use a more up to date browser or turn off compatibility mode in Internet Explorer. In the meantime, to ensure continued support, we are displaying the site without styles and JavaScript. The interpretation proposed so far invokes the internal instability resulting from the large-scale interaction between upper and interior oceanic layers.

Here we show, using a new high-resolution simulation of the realistic North Pacific Ocean, that ocean eddies are instead sustained by a different process that involves small-scale mixed-layer instabilities set up by large-scale atmospheric forcing in winter. This leads to a seasonal evolution of the eddy kinetic energy in a very large part of this ocean, with an amplitude varying by a factor almost equal to 2.

Perspectives in terms of the impacts on climate dynamics and future satellite observational systems are briefly discussed. As such, it is driven by nonlinear scale interactions that can transfer energy upscale or downscale. KE associated with mesoscale eddies is monitored from space by satellite altimeters and these eddies are also explicitly resolved in present-day realistic ocean numerical simulations. Until recently, the broadly accepted paradigm is that these eddies are generated and sustained by the instability of the large-scale vertical current shear or horizontal gradient of quasigeostrophic potential vorticity QGPV in the ocean interior.