نتایج جستجو برای: scale climatic signals including ocean

تعداد نتایج: 1723610  

2008
Oli G. B. Sveinsson Jocelyn Gaudet Yochanan Kushnir Vincent Fortin

Results from diagnostic analyses to understand the seasonal evolution of the large-scale climatic state responsible for the development and melt of the winter snowpack, and spring–early summer precipitation in the Churchill Falls region on the QuébecLabrador Peninsula, Canada, are presented in the context of the development of an empirical model for seasonal to annual streamflow forecasting, wi...

2017
Kenji Kawamura Ayako Abe-Ouchi Hideaki Motoyama Yutaka Ageta Shuji Aoki Nobuhiko Azuma Yoshiyuki Fujii Koji Fujita Shuji Fujita Kotaro Fukui Teruo Furukawa Atsushi Furusaki Kumiko Goto-Azuma Ralf Greve Motohiro Hirabayashi Takeo Hondoh Akira Hori Shinichiro Horikawa Kazuho Horiuchi Makoto Igarashi Yoshinori Iizuka Takao Kameda Hiroshi Kanda Mika Kohno Takayuki Kuramoto Yuki Matsushi Morihiro Miyahara Takayuki Miyake Atsushi Miyamoto Yasuo Nagashima Yoshiki Nakayama Takakiyo Nakazawa Fumio Nakazawa Fumihiko Nishio Ichio Obinata Rumi Ohgaito Akira Oka Jun'ichi Okuno Junichi Okuyama Ikumi Oyabu Frédéric Parrenin Frank Pattyn Fuyuki Saito Takashi Saito Takeshi Saito Toshimitsu Sakurai Kimikazu Sasa Hakime Seddik Yasuyuki Shibata Kunio Shinbori Keisuke Suzuki Toshitaka Suzuki Akiyoshi Takahashi Kunio Takahashi Shuhei Takahashi Morimasa Takata Yoichi Tanaka Ryu Uemura Genta Watanabe Okitsugu Watanabe Tetsuhide Yamasaki Kotaro Yokoyama Masakazu Yoshimori Takayasu Yoshimoto

Climatic variabilities on millennial and longer time scales with a bipolar seesaw pattern have been documented in paleoclimatic records, but their frequencies, relationships with mean climatic state, and mechanisms remain unclear. Understanding the processes and sensitivities that underlie these changes will underpin better understanding of the climate system and projections of its future chang...

2011
S. Adeli

Crater degradation on Mars is a key to understand erosion through time. Strongly eroded craters in the highlands are interpreted to be the result of enhanced erosion rate during the Noachian epoch [1]. While fluvial valleys climatic meaning and duration are still difficult to define (strongly warmer climate or episodic activity under slightly warmer climate), the enhanced Noachian craters degra...

Journal: :جغرافیا و مخاطرات محیطی 0
دل آرام هوشمند محمد جواد خردادی

. introduction global warming and its result, climate change is an important subject investigated especially in the recent decades by researchers throughout the world. in these studies, at first, climatic parameters changes are investigated. considering many uncertainties in the parameters estimation, it is better to choose a method in order to study and analyze the uncertainty band due to diff...

2017
Germain Bayon Patrick De Deckker John W. Magee Yoan Germain Sylvain Bermell Kazuyo Tachikawa Marc D. Norman

Millennial-scale cooling events termed Heinrich Stadials punctuated Northern Hemisphere climate during the last glacial period. Latitudinal shifts of the intertropical convergence zone (ITCZ) are thought to have rapidly propagated these abrupt climatic signals southward, influencing the evolution of Southern Hemisphere climates and contributing to major reorganisation of the global oceanatmosph...

Journal: :Molecular ecology 2012
Ana R Amaral Luciano B Beheregaray Kerstin Bilgmann Luís Freitas Kelly M Robertson Marina Sequeira Karen A Stockin M M Coelho Luciana M Möller

Climatic oscillations during the Pleistocene have greatly influenced the distribution and connectivity of many organisms, leading to extinctions but also generating biodiversity. While the effects of such changes have been extensively studied in the terrestrial environment, studies focusing on the marine realm are still scarce. Here we used sequence data from one mitochondrial and five nuclear ...

Journal: :Paleoceanography and paleoclimatology 2021

Tectonics and regional monsoon strength control weathering erosion regimes of the watersheds feeding into Bay Bengal, which are important contributors to global climate evolution via carbon cycle feedbacks. The detailed mechanisms controlling input terrigenous clay Bengal on tectonic orbital timescales are, however, not yet well understood. We produced orbital-scale resolution geochemical recor...

2006
Philip F. Sexton Paul A. Wilson Richard D. Norris

[1] Until recently, very few high-quality deep ocean sedimentary sections of Eocene age have been available. Consequently, our understanding of Eocene paleoceanography has become heavily reliant on ‘‘composite’’ records patched together from multiple sites in different ocean basins and generated using multiple taxa (potential sources of ‘‘local’’ noise in the global signal). Here we test the re...

2007
Didier M. Roche Hans Renssen Susanne L. Weber Hugues Goosse

[1] The lack of climatic imprint left by the Meltwater Pulse-1A (’14.5 ka BP), equivalent to a sea-level rise of 14 to 20 meters, is puzzling. Recent studies suggest the event might have occurred as a hyperpycnal flow in the Gulf of Mexico, preventing its detection in oceanic records throughout the North Atlantic. We present a suite of simulations with the LOVECLIM climate model, which mimic th...

2008
Hanno Sandvik Kjell Einar Erikstad H. Sandvik

In the light of the predicted changes in climate as a consequence of global warming, it is a major concern how animal species will respond to altered meteorological and oceanographic conditions. Seabirds constitute a diverse group of marine top predators which have relatively low fecundity and high annual survival rates. In order to predict effects of climate change, it is a necessary precondit...

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