In this theory, larger-bodied individuals will be unable to compensate for increased metabolic demands associated with high temperature due to the gills providing decreasing amounts of oxygen per unit body mass. As a result, fishes will reach maximum size when their gills can only meet the ...
ensuring a good night’s rest. You’ll find the room sits at a very comfortable temperature, and the air conditioning works wonders. The L shaped lounge in the corner is also a great place to relax and watch TV at the end of the day. ...
Department of Oceanography, University of Hawaii, HonoluluAmerican Society of Limnology and OceanographyDeep Sea Research and Oceanographic AbstractsWyrtki, K. 1965 . The annual and semiannual variation of sea surface temperature in the North Pacific Ocean. Limnology and Oceanography 10: 307 – 313. ....
Oceanic processes in ocean temperature products key to a realistic presentation of positive Indian Ocean Dipole nonlinearity. Geophys. Res. Lett. 47, e2020GL089396 (2020). Article Google Scholar An, S.-I. et al. Main drivers of Indian Ocean Dipole asymmetry revealed by a simple IOD model....
Signatures of the Antarctic ozone hole in Southern Hemisphere surface climate change. Nat. Geosci. 4, 741–749 (2011). Article CAS Google Scholar Kostov, Y. et al. Fast and slow responses of Southern Ocean sea surface temperature to SAM in coupled climate models. Clim. Dyn. 48, 1595–...
S., Temporal and spatial variations of the temperature and sound speed in the Tongue of the Ocean, Bahamas. [unpubl]. Ms.- Inform. Manuscr. U.S. nav. oceanogr. Off. IM No. 66-5,1966. 10 S. m. Abb. Winokur, R. S., Chanesman, S., A pulse method for sound speed ...
Over the past half a century, both the Indian Ocean (IO) and the North Atlantic Ocean (NA) exhibit strong warming trends like a global mean surface temperature (SST). Here, we show that not only simply as a result of increased greenhouse gases, but the I
Dissolved oxygen (µmol O2 kg−1; black, left y-axis) and temperature (°C; blue, right y-axis) as a function of time in order of sites with increasing deployment length, ranging from 3 to 309 days (Supplementary Table 1). For each location, different instrument deployment sites are...
(Methods). The pre-genesis TCs modify the ocean potential temperature profiles down to approximately 200 m. Even at greater depths, their influence is still noticeable, though weaker (Fig.4aand Supplementary Fig.3). Moreover, TC-induced temperature changes reach deeper in the context of deep...
Braithwaite, W. R. The calculation of minimum safe inspired gas temperature limits for deep diving. U. S. Navy Exp. Diving Unit, Rep. NEDU 12-72 (July 1972). Google Scholar Brauer, R. W. Narrative account of a series of pressure chamber dives reaching to 1190 ft. in search of speci...