Third interim report pursuant to S. Res, 202, 81st Congress, a resolution to investigate gambling and racketeering activities.

Mode of access: Internet.

"U 202"; kriegstagebuch, angefangen den 12. april 19.., abgeschlossen den 30. april 19.

51. bis 100. tausend.

The Economic impact of proposed regulation R82-1 : remanded particulate regulations 203 (g) (1) and 202 (b) /

Project no. EA44.

Field and depot maintenance manual : engine, gasoline, fuel injected, supercharged, horizontal-opposed, air cooled, six cylinder, assembly-2805-528-6015, (Continental model AOSI-895-5 and AOSI-895-5M) : end item application : gun, self-propelled, full tracked, twin 40-mm, M42A1 (TM 9-2350-202), howitzer, self-propelled, full tracked, 105-mm, M52A1 (TM 9-2350-209) ....

Includes index.

Intercommunication stations, LS-200/FI, LS-201/FI, LS-202/FI, and LS-125B/FI.

"August 1955."

Lists of wage stabilization cases acted on by the Headquarters Office of the National War Labor Board, 1942-45 [Record group 202]

Cover title.

Investigation of strike in steel industries : hearings before the Commmittee on Education and Labor, United States Senate, Sixty-sixth Congress, first session pursuant to S. Res. 202 on the resolution of the Senate to investigate the strike in steel industries.

The title page for Part 2 says "S. Res. 188, Instructing the Committee on Education and Labor of the United States Senate to investigatethe strike of the employees of the steel mills of the United States, and so forth and S. Res. 202, authorizing the Committee on Education and Labor, in its investigation of the steel strike, to hold hearings, to employ a stenographer, to require the attendance of witnesses and the production of papers, documents, and so forth, and prescribing penalties for the refusal of witnesses to attend or answer questions."

Isotope and Mg/Ca measurements from Cores ME0005A-43JC and 202-1242 of tropical Pacific

Multiproxy geologic records of d18O and Mg/Ca in fossil foraminifera from sediments under the Eastern Pacific Warm Pool (EPWP) region west of Central America document variations in upper ocean temperature, pycnocline strength, and salinity (i.e., net precipitation) over the past 30 kyr. Although evident in the paleotemperature record, there is no glacial-interglacial difference in paleosalinity, suggesting that tropical hydrologic changes do not respond passively to high-latitude ice sheets and oceans. Millennial variations in paleosalinity with amplitudes as high as 4 practical salinity units occur with a dominant period of 3-5 ky during the glacial/deglacial interval and 1.0-1.5 ky during the Holocene. The amplitude of the EPWP paleosalinity changes greatly exceeds that of published Caribbean and western tropical Pacific paleosalinity records. EPWP paleosalinity changes correspond to millennial-scale climate changes in the surface and deep Atlantic and the high northern latitudes, with generally higher (lower) paleosalinity during cold (warm) events. In addition to Intertropical Convergence Zone (ITCZ) dynamics, which play an important role in tropical hydrologic variability, changes in Atlantic-Pacific moisture transport, which is closely linked to ITCZ dynamics, may also contribute to hydrologic variations in the EPWP. Calculations of interbasin salinity average and interbasin salinity contrast between the EPWP and the Caribbean help differentiate long-term changes in mean ITCZ position and Atlantic-Pacific moisture transport, respectively.

Stable carbon and oxygen isotopes and Mg/Ca ratios of foraminifers from ODP Site 202-1241 sediments

A combination of stable isotope records and Mg/Ca temperature estimates of four different planktonic foraminiferal species from Ocean Drilling Program Site 1241 allows differentiation between temperature and salinity changes in the tropical east Pacific (TEP) upper water column during the Pliocene (~5.7-2.1 Ma). The deviation of d18O records and Mg/Ca temperature estimates from thermocline-dwelling planktonic foraminifers suggests that local changes in salinity exerted a much stronger control on Pliocene TEP upper ocean water mass signatures than previously assumed. The most pronounced Pliocene change in TEP upper ocean stratification was the shoaling of the thermocline from ~4.8 to 4.0 Ma that was possibly triggered by changes in the configuration of low-latitude ocean gateways. During this time interval, mixed-layer temperatures and salinities remained relatively constant in contrast to a pronounced temperature (~6°C) and salinity decrease at the bottom of the photic zone. This change led to a new state in the thermal structure of the TEP, as the thermocline remained relatively shallow until ~2.1 Ma.