Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Huaxiao Wang"'
Autor:
Kaihua Wu, Xiaoyan Liang, Xiu Zhang, Guoping Yang, Huaxiao Wang, Yining Xia, Shumila Ishfaq, Hongfei Ji, Yuxi Qi, Wei Guo
Publikováno v:
Frontiers in Plant Science, Vol 15 (2024)
Salt stress is a well-known abiotic constraint that hampers crop productivity, affecting more than 424 million hectares of topsoil worldwide. Applying plant growth regulators externally has proven effective in enhancing crop resilience to salt stress
Externí odkaz:
https://doaj.org/article/08c5293579394ee1b578c7a307f4ce3a
Publikováno v:
Zhonghua jie he he hu xi za zhi = Zhonghua jiehe he huxi zazhi = Chinese journal of tuberculosis and respiratory diseases. 37(1)
Autor:
Edward C. Wiebe, Amy MacFadyen, Andrew J. Weaver, Andreas Schmittner, P. B. Duffy, Augustus F. Fanning, H. Damon Matthews, Tracy Ewen, Cecilia M. Bitz, Michael Eby, Marika M. Holland, Huaxiao Wang, Masakazu Yoshimori, Oleg A. Saenko, Katrin J. Meissner
Publikováno v:
Atmosphere-Ocean. 39:361-428
A new earth system climate model of intermediate complexity has been developed and its climatology compared to observations. The UVic Earth System Climate Model consists of a three‐dimensional ocean general circulation model coupled to a thermodyna
Autor:
Sigfus J Johnsen, Lloyd D Keigwin, Richard B. Alley, Joseph M. Licciardi, Huaxiao Wang, Peter U. Clark
Publikováno v:
Paleoceanography. 11:563-577
Well-dated sea level records show that the glacioeustatic rise following the last glacial maximum was characterized by two or possibly three brief intervals of rapid sea level rise separating periods with much lower rates. These very high rates of se
Autor:
G. E. Birchfield, Huaxiao Wang
Publikováno v:
Climate Dynamics. 8:49-53
Latitudinal heat transport in the ocean and atmosphere represents a fundamental process of the Earth's climate system. The ocean component of heat transport is effected by the thermohaline circulation. Changes in this circulation, and hence latitudin
Publikováno v:
Journal of Marine Systems. 1:197-208
A coupled ocean-atmosphere box model is presented which, although extremely simplified, permits study of the time domain response of a model of the Atlantic Ocean coupled to an atmosphere. In particular the model can be used to systematically examine
Publikováno v:
Paleoceanography. 5:383-395
The importance of the hydrological cycle as a controlling factor on the magnitude of the thermohaline circulation is illustrated in a simple one-hemisphere coupled ocean-atmosphere box model. The ocean model includes differential surface heating and
Publikováno v:
Ice in the Climate System ISBN: 9783642850189
Rapid climate changes (Dansgaard-Oeschger events) during most of the last glaciation and during the last deglaciation, seen in the Greenland ice cores and a deep sea sediment core in the North Atlantic, are likely caused by dynamical instability of t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a1819251f4ef2d3b083088e9bb529aba
https://doi.org/10.1007/978-3-642-85016-5_15
https://doi.org/10.1007/978-3-642-85016-5_15
Publikováno v:
Journal of Geophysical Research. 99:12459
We demonstrate in a simple climate model that there exist nonlinear feedbacks between the atmosphere, ocean, and ice sheets capable of producing century/millennium timescale internal oscillations resembling those seen in the paleoclimate record. Feed
Autor:
Weaver, Andrew J., Eby, Michael, Wiebe, Edward C., Bitz, Cecilia M., Duffy, Phil B., Ewen, Tracy L., Fanning, Augustus F., Holland, Marika M., MacFadyen, Amy, Matthews, H. Damon, Meissner, Katrin J., Saenko, Oleg, Schmittner, Andreas, Huaxiao Wang, Yoshimori, Masakazu
Publikováno v:
Atmosphere - Ocean (Canadian Meteorological & Oceanographic Society); Dec2001, Vol. 39 Issue 4, p361-428, 68p