Figure S1. SSHA around station KEO before, when and after the cyclonic eddy #1 and #2 (CE1 and CE2, respectively) passed over station KEO. (PDF 714Â kb
The chemistry and biology of the ocean are superimposed on the ocean's circulation, thus it is ...
Spatial distribution of the average annual mean temperature in °C in NHAR for the period 1980â201...
Table S1. Bioclimatic variables (BIO1 to BIO19) from WorldClim [51]. Variables marked with an asteri...
Figure S2. Profile time-series of seawater temperature (°C) in the upper ocean above ~ 550 m at stat...
Figure S4. Hourly time-series of surface pressure (hPa, red line) and ocean current vector at 36 m d...
Figure S3. Tracks of typhoons during experimental 2Â years. Lines with open circle, square, triangle...
Figure S5. Vertical profile of NO3 in the subtropical region near KEO in September. Data of respecti...
In 2014, a sediment trap mooring was deployed adjacent to station Kuroshio Extension Observatory (KE...
Cyclonic and anticyclonic eddies are usually characterized by upwelling and downwelling, respectivel...
5 pages. -- This PDF file includes: Figs. S1 to S2. -- Tables S1 to S2.Peer reviewe
Rankings of loadings for the first two principal components (PC1, PC2) of 604 Bulbophyllum clade C (...
Change in atmospheric variables due to 1Â K SST warming in the WSST region from 1982 to 2012 for hig...
and ecosystems Using a high resolution model, the Ocean general circulation model For the Earth Simu...
Mesoscale eddies (MEs) affect the transport and redistribution of oceanic matter and energy. The lon...
The European Centre for Medium-Range Weather Forecasts Tropical Ocean–Global Atmosphere advanced ana...
The chemistry and biology of the ocean are superimposed on the ocean's circulation, thus it is ...
Spatial distribution of the average annual mean temperature in °C in NHAR for the period 1980â201...
Table S1. Bioclimatic variables (BIO1 to BIO19) from WorldClim [51]. Variables marked with an asteri...
Figure S2. Profile time-series of seawater temperature (°C) in the upper ocean above ~ 550 m at stat...
Figure S4. Hourly time-series of surface pressure (hPa, red line) and ocean current vector at 36 m d...
Figure S3. Tracks of typhoons during experimental 2Â years. Lines with open circle, square, triangle...
Figure S5. Vertical profile of NO3 in the subtropical region near KEO in September. Data of respecti...
In 2014, a sediment trap mooring was deployed adjacent to station Kuroshio Extension Observatory (KE...
Cyclonic and anticyclonic eddies are usually characterized by upwelling and downwelling, respectivel...
5 pages. -- This PDF file includes: Figs. S1 to S2. -- Tables S1 to S2.Peer reviewe
Rankings of loadings for the first two principal components (PC1, PC2) of 604 Bulbophyllum clade C (...
Change in atmospheric variables due to 1Â K SST warming in the WSST region from 1982 to 2012 for hig...
and ecosystems Using a high resolution model, the Ocean general circulation model For the Earth Simu...
Mesoscale eddies (MEs) affect the transport and redistribution of oceanic matter and energy. The lon...
The European Centre for Medium-Range Weather Forecasts Tropical Ocean–Global Atmosphere advanced ana...
The chemistry and biology of the ocean are superimposed on the ocean's circulation, thus it is ...
Spatial distribution of the average annual mean temperature in °C in NHAR for the period 1980â201...
Table S1. Bioclimatic variables (BIO1 to BIO19) from WorldClim [51]. Variables marked with an asteri...