137,026 research outputs found
Sanford Bates Correspondence from L. N. Yepsen
No full textA letter addressed to Sanford Bates from L. N. Yepsen concerning the American Association on Mental Deficiency annual meeting and Bates' responsibilities
Sanford Bates Correspondence from L. N. Yepsen Page 2
No full textThe second page of a letter addressed to Sanford Bates from L. N. Yepsen concerning the American Association on Mental Deficiency annual meeting and Bates' responsibilities
Sanford Bates Correspondence from L. N. Yepsen Page 1
No full textThe first page of a letter addressed to Sanford Bates from L. N. Yepsen concerning the American Association on Mental Deficiency annual meeting and Bates' responsibilities
Sanford Bates Correspondence from Nicholas N. Kittrie
No full textA letter addressed to Sanford Bates from Nicholas N. Kittrie in which Kittrie announces he is leaving as Director of the Project on the Rights of the Mentally Ill
Sanford Bates Correspondence from Nicholas N. Kittrie Page 2
No full textThe second page of a letter addressed to Sanford Bates from Nicholas N. Kittrie
Sanford Bates Correspondence from Nicholas N. Kittrie Page 1
No full textThe first page of a letter addressed to Sanford Bates from Nicholas N. Kittrie
Sanford Bates Correspondence to "Will"
No full textA letter addressed to "Will" from Sanford Bates concerning copies of Will's N. P. P. A. statement. Part of this letter is missing, the page appears cut off
Multi-decadal uptake of carbon dioxide into subtropical mode water of the North Atlantic Ocean
No full textNatural climate variability impacts the multi-decadal uptake of anthropogenic carbon dioxide (Cant) into the North Atlantic Ocean subpolar and subtropical gyres. Previous studies have shown that there is significant uptake of CO2 into subtropical mode water (STMW) of the North Atlantic. STMW forms south of the Gulf Stream in winter and constitutes the dominant upper-ocean water mass in the subtropical gyre of the North Atlantic Ocean. Observations at the Bermuda Atlantic Time-series Study (BATS) site near Bermuda show an increase in dissolved inorganic carbon (DIC) of +1.51±0.08 ?mol kg?1 yr?1 between 1988 and 2011, but also an increase in ocean acidification indicators such as pH at rates (?0.0022±0.0002 yr?1) higher than the surface ocean (Bates et al., 2012). It is estimated that the sink of CO2 into STMW was 0.985±0.018 Pg C (Pg=10 15gC) between 1988 and 2011 (70±1.8 % of which is due to uptake of Cant). The sink of CO2 into the STMW is 20 % of the CO2 uptake in the North Atlantic Ocean between 14?–50? N (Takahashi et al., 2009). However, the STMW sink of CO2 was strongly coupled to the North Atlantic Oscillation (NAO), with large uptake of CO2 into STMW during the 1990s during a predominantly NAO positive phase. In contrast, uptake of CO2 into STMW was much reduced in the 2000s during the NAO neutral/negative phase. Thus, NAO induced variability of the STMW CO2 sink is important when evaluating multi-decadal changes in North Atlantic Ocean CO2 sinks
Sanford Bates Correspondence from Ella Ulman
No full textA letter addressed to Sanford Bates from Ella Ulman expressing her gratitude for his assistance with her late husband's memorial, Judge Joseph N. Ulman
Sanford Bates Correspondence to Bernard W. Kofsley
No full textA handwritten letter addressed to Bernard W. Kofsley from Sanford Bates concerning previous correspondence and an address to the U. N. Congress
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