Future change of the Indian Ocean basin-wide and dipole modes in the CMIP5. Climate Dynamics, 43(1--2): 535--551Chu, J.-E., and Coauthors, 2014: Future change of the Indian Ocean basin- wide and dipole modes in the CMIP5. Clim. Dynam., 43, 535-551, doi: 10.1007/s00382-013...
The combined effect of the planetary Rossby wave and the topographic Rossby wave results in a basin-wide barotropic sea level fluctuation that ranges from the northern boundary of the Indian Ocean to the Southeast Indian ridge. The continental shelf wave, in contrast, appears to play no role in...
The Indian Ocean sea surface temperature (SST) variability has been represented with the two dominant variability modes: the Indian Ocean basin-wide (IOBW) and dipole (IOD) modes. Here we investigate future changes of the two modes together with mean state and El Nio and Southern Oscillation (...
3) simulation of tsunami in Indian Ocean 印度洋海啸模拟4) basin-wide mode 海盆模态 1. The "charge/discharge" roles of the basin-wide mode of the Indian Ocean SST anomaly——influence on the South Asian High in summer; 热带印度洋SST海盆模态的“充电/放电”作用——对夏季南亚高压的影响...
2002 . Signals of interannual and interdecadal variability of air–sea interaction in the basin-wide Indian Ocean . Atmosphere–Ocean 40 ( 3 ): 293 – 311 .Qian Weihong,Hu H.R,Deng Y.Signals of interannual and interdecadal variability of air-sea interaction in the basin-wide Indian Ocean....
The tropical Indian Ocean has experienced rapid basin-wide sea surface temperature (SST) warming, with an average rise of 1.0 °C (0.15 °C/decade) during 1951–2015, over which period the global average SST warmed about 0.7 °C (0.11 °C/decade) (high confidence). The SST warming is ...
Summary Characterizing how the Indian Ocean dipole (IOD) modifies typical basin-wide dynamical variability has been vigorously pursued over the past decade. Along with this dynamic response, a clear biological impact has been revealed in the ocean color data acquired by remote sensing platforms such ...
basin-wide warming during the final phase (70‒100 years) (Supplementary Fig.9b). The enhanced meridional sea surface salinity gradient and AMOC due to IO warming (Supplementary Fig.10) could increase the northward transport of ocean heat, which subsequently would warm the entire North Atlantic...
Continuous remote-sensed daily fields of ocean color now span over two decades; however, it still remains a challenge to examine the ocean ecosystem processes, e.g., phenology, at temporal frequencies of less than a month. This is due to the presence of significantly large gaps in satellite ...
The weakening of zonal atmospheric circulation, a widely accepted projection of climate change in response to global warming, features a weakening of the Indian Ocean Walker circulation (IWC), with an anomalous ascending motion over the western and anoma