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Ocean Acidification: The Other CO2 Problem
Ocean acidification is a predictable consequence of rising atmospheric CO 2 and does not suffer from uncertainties associated with climate change forecasts. Absorption of anthropogenic CO 2, reduced pH, and lower calcium carbonate (CaCO 3) saturation in surface waters, where the bulk
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IMO | ISM Code
www.ocean.washington.edu1.1.6 Safety Management Certificate means a document issued to a ship which signifies that the Company and its shipboard management operate in accordance with the approved safety management system. 1.1.7 Objective evidence means quantitative or qualitative information, records or statements of fact pertaining to safety or to the existence and implementation of a …
Chpt 4: Major Ions of Seawater James Murray (10/01/04 ...
www.ocean.washington.edu9 shown in Fig. 4-8 (from Becks et al., 1992). Beck et al (1992) and Guilderson et al (1994) used Sr/Ca results from corals to suggest that the tropical western Pacific and western Atlantic were 4°C and 6°C cooler during the last glacial maximum (LGM) than today. Fig 4-8 Sr/Ca versus temperature for scleractinian corals (Beck et al., 1992)
8. Cross-Correlation Cross-correlation
www.ocean.washington.eduzero or negative indexes the cross correlation sample with zero lag is the central element in the output vector. An alternate way of doing the cross correlation without padding with zeros is using the conv command (phixy = conv(y,x(end:-1:1))) ESS 522 2014 8-2 Autocorrelation
Chpt. 3: Properties of Water and Seawater James W. Murray ...
www.ocean.washington.eduChpt. 3: Properties of Water and Seawater James W. Murray (9/30/04) Univ. Washington I. The Nature of pure water Seawater is composed mostly of water (H2O). In fact it is about 96.5 wt % water. Sediments are also mostly water. Most fine grained surface sediments have a porosity
Chapter 6 Activity Scales and Activity Corrections (10/11 ...
www.ocean.washington.eduthus the activity (a), are equal to one (e.g., Ci = γi = ai = 1), and thus the log terms are equal to zero. Then µi = µi°(T,P). The reference state is the solution limit where Ci = ai and thus γi = 1. The choice of reference states determined the value of the activity coefficient, γi. The differences in the activity scales show up as ...
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