From webserver@lib.washington.edu Fri Jul 6 14:56:58 2001 Date: Tue, 03 Jul 2001 13:31:58 -0700 From: webserver@lib.washington.edu To: scottv@ocean.washington.edu Subject: peter saunders refs Search History * #17 (saunders-pm) in AU (26 records) #16 saunders and peter (1 record) #15 saunders peter and (PY=1994-1994) (0 records) #14 #2 and #13 (1 record) #13 saunders and (PY=1994-1994) (139 records) #12 ((saj ) in AU) in AU (112 records) #11 ((saj ) in AU) in AU (112 records) #10 (saunders p m) in AU (0 records) #9 (saunders-p-m) in AU (0 records) #8 #1 and #6 (15 records) #7 #5 and #6 (0 records) #6 topography (45177 records) #5 #1 and #2 (95 records) #4 #1 and #3 (4 records) #3 francis (4304 records) #2 flow (328129 records) #1 (saunders) in AU (2358 records) Record 1 of 26 in INSPEC 1999/01-1999/10 TI: Circulation of the Pacific Ocean seen in a global ocean model: Ocean Circulation and Climate Advanced Modelling Project (OCCAM) AU: Saunders-PM; Coward-AC; de-Cuevas-BA SO: Journal-of-Geophysical-Research. vol.104, no.C8; 15 Aug. 1999; p.18281-99 PY: 1999 LA: English AB: Compares observations made in the Pacific Ocean and the 8-12 year climatology of a global numerical model. Meridional mass and heat transports and their divergences are calculated, and zonal averages compared with the air-sea exchange values of Doney et al. (1998) with mixed success. The large scale distribution of sea surface height and near-surface currents are shown to be well reproduced by the model, but their variance is underestimated, severely so in areas of weak variability. Synoptic wind forcing enhances the latter, though only slightly, while higher model resolution improves agreement in areas of strong variability. Model mean transports in the East Australian Current, in the Vitiaz Strait and in the Kuroshio exceed measurements by 10, 0, 18 Sv, respectively, and variability is underestimated by factors between 2 and 4. Near 1000 m and in strong currents the flow is overestimated, but over most of the ocean, model output does not match either the magnitude or ! the spatial variability of the observations. In contrast, the inflow of bottom water and its spreading path throughout both the South and North Pacific is well described. Good agreement is found with measured transport through the Samoan Passage, but at 32 degrees S, east of the Tonga-Kermadec Ridge, the model yields only 60% of the observed value. The Sverdrup balance is shown to hold widely in the model interior. Utilizing the complete depth-integrated vorticity equation it is found that bottom pressure torques balance the advection of planetary vorticity in both surface and bottom intensified western boundary currents. DE: oceanographic-regions MN: J047-1999-056 AN: 6373479 *LHM: See records of latest issues received http://catalog.lib.washington.edu/record=b2037688 Location: null -- Call number: 538.705 TE Sec.C -- LIB HAS: v.83-104 (1978-1999) -- Sec.C (Oceans) Location: null -- Call number: 538.705 TE -- LIB HAS: v.64-v.82 (1959-1977) Location: Fish-Ocean Stacks -- Call number: 538.705 TE Sec.C -- LIB HAS: v.105- (2000-) -- Sec.C (Oceans); LATEST ISSUES ON DISPLAY Location: NatSci Periodicals -- Call number: 538.705 TE -- LIB HAS: v.54- (1949-) -- LATEST ISSUES ON DISPLAY Record 2 of 26 in INSPEC 1996 TI: The flux of dense cold overflow water southeast of Iceland AU: Saunders-PM SO: Journal-of-Physical-Oceanography. vol.26, no.1; Jan. 1996; p.85-95 PY: 1996 LA: English AB: From the period commencing midsummer 1990 and lasting for 13 months, 13 current meters were deployed on seven moorings at depths between 1000 and 2300 m southeast of Iceland (63 degrees 09'N, 17 degrees 18'W to 61 degrees 44'N, 15 degrees 24'W). The purpose of the array (designated WOCE ACM8) was to measure the overflow of dense water, downstream of the source in the Faeroe Bank Channel and downstream of any sources on the Iceland-Faeroe Ridge. In the depth range 1300-2100 m three of the moorings showed a bottom intensified current that was persistent and directed to the southwest; at the other moorings the current was erratic and weak. The records were combined to form a transport time series for water denser than sigma /sub o/>27.8 kg m/sup -3/ in the direction 240 degrees . A mean value of 3.2+or-0.5 Sv was found with considerable variability near a period of seven days, but there was no convincing evidence for a seasonal signal. The amount of pure Norwegian Sea wate! r present in the overflow was estimated at 1.6+or-0.15 Sv, close to previous determinations and comparable to that measured in the Faeroe Bank Channel. A small contribution is therefore deduced as crossing the Iceland-Faeroe Ridge. A general freshening of the water column in the northern Iceland Basin in the period 1960-1990 is demonstrated. DE: oceanographic-regions MN: J181-96002 AN: 5428188 *LHM: Connect to this title online; UW restricted http://ams.allenpress.com/amsonline/?request=get-archive&issn=1520-0485 See records of latest issues received http://catalog.lib.washington.edu/record=b2038065 Location: Available Online Location: Available Online -- Shelved by title: Full Text through ProQuest Direct http://proquest.umi.com/pqdlink?Ver=1&Exp=07-01-2003&REQ=3&Cert=7YMWy6YMy6bpLgoHt04CRpK0odiyGY8GFyPJRYCOyb4QcDP5iYc3XsCDREiVdG8Y&Pub=36166 -- LIB HAS: Jun.1998- -- Restricted to UW, and other Cooperative Library Project institutions. This title is purchased as part of the Cooperative Library Project. Location: Fish-Ocean Stacks -- Call number: GC1 .J68 -- LIB HAS: v.1- (1971-) -- Latest issues on display Record 3 of 26 in INSPEC 1996 TI: Oceanic fluxes on the WOCE A11 section AU: Saunders-PM; King-BA SO: Journal-of-Physical-Oceanography. vol.25, no.9; Sept. 1995; p.1942-58 PY: 1995 LA: English AB: The most southerly WOCE one-time section in the South Atlantic, designated A11, was occupied in January 1993. The cruise track lay across the cool subantarctic zone of the Circumpolar Current in the west and the warm subtropical gyre in the east. In this paper estimates of the flux of heat, salt, oxygen, and other tracers across the section are presented. A brief description of the distribution of physical and chemical properties is followed by a determination of the flux in the surface Ekman layer. Direct measurements of current shear made from a shipborne ADCP and estimates from cruise wind data and climatological data all yield a flux of 5+or-1 Sv (Sv identical to 10/sup 6/ m/sup 3/ s/sup -1/) equatorward. When combined with geostrophic estimates relative to a level near 3500 dbar, or the bottom where shallower, an initial guess for the flow field is derived. This initial guess is combined with absolute currents derived from the ADCP when the ship is underway. Unreal! istic aspects of the circulation are found, and the authors conclude that the ageostrophic "noise" of the ADCP measurements is to blame. A second and preferred flow field is derived using an inverse analysis supplemented by a few estimates of total current transports. Climatological transports in the Falkland Current are estimated at about 45 Sv equatorward, while on the eastern margin a poleward transport of about 5 Sv is assumed. The equatorward flux of bottom water is taken from a recent determination to be 6 Sv. The heat flux estimate across the section is found to be robust and to have twice the value reported recently. The flux is equatorward with magnitude of 0.5+or-0.1 PW and occurs entirely within the subtropical gyre. A net equatorward transport of 10 Sv of upper thermocline water, which takes place near the eastern margin, has also been inferred. This pair of estimates identifies the warm water path as the route for the upper-ocean replacement of NADW. The flux of! salt, for zero volume transport across the section, is found! to be 0+or-5 Sv psu ( 1 Sv psu approximately=10/sup 6/ kg s/sup -1/) and when interpreted as a freshwater flux is quite at variance with estimates based on the global freshwater balance. Oxygen and other nutrients have fluxes generally differing in sign from previous determinations. Sensitivity of the results to assumptions made is considered. DE: oceanographic-regions MN: J181-95011 AN: 5395943 *LHM: Connect to this title online; UW restricted http://ams.allenpress.com/amsonline/?request=get-archive&issn=1520-0485 See records of latest issues received http://catalog.lib.washington.edu/record=b2038065 Location: Available Online Location: Available Online -- Shelved by title: Full Text through ProQuest Direct http://proquest.umi.com/pqdlink?Ver=1&Exp=07-01-2003&REQ=3&Cert=7YMWy6YMy6bpLgoHt04CRpK0odiyGY8GFyPJRYCOyb4QcDP5iYc3XsCDREiVdG8Y&Pub=36166 -- LIB HAS: Jun.1998- -- Restricted to UW, and other Cooperative Library Project institutions. This title is purchased as part of the Cooperative Library Project. Location: Fish-Ocean Stacks -- Call number: GC1 .J68 -- LIB HAS: v.1- (1971-) -- Latest issues on display Record 4 of 26 in INSPEC 1996 TI: Bottom currents derived from a shipborne ADCP on WOCE cruise A11 in the South Atlantic AU: Saunders-PM; King-BA SO: Journal-of-Physical-Oceanography. vol.25, no.3; March 1995; p.329-47 PY: 1995 LA: English AB: This paper is divided into two parts: the first describing an enhancement of the shipborne ADCP system and the second describing information about bottom currents that have been obtained there from on WOCE cruise A11 in the South Atlantic, Punta Arenas to Cape Town. RRS Discovery has been fitted with a GPS3DF receiver and an array of antennas about its bridge, which determine the instantaneous attitude of the ship. The heading record from this instrument has been compared with the ship's gyrocompass throughout the 40-day cruise. Differences have been calculated and examined according to heading, speed, and movements. Underway differences are found insensitive to heading except in a southerly sector, but on station, differences exhibit a sinusoidal dependence on heading with range 3 degrees . Steaming from a station led to transient behavior with recognizable effects for 1 hour. The results are generally consistent with earlier reports and are attributed to gyro error. A! n improved heading measurement has a marked effect on currents determined from the ADCP when under way. The cruise data from this instrument has been reprocessed, replacing the observations of the gyrocompass with those from the GPS3DF unit. The authors describe and implement the procedure for dealing with two difficulties, namely, gaps in the data and misalignment of the two pieces of equipment. An estimate of the current error from known causes is found to be only 1 cm s/sup -1/ for 4-h steaming or station averages. A comparison of the ADCP cross-track component with geostrophic estimates referenced to the bottom for 91 stations shows excellent overall agreement, both for underway and station-pair measurements. Differences are principally due to transient ageostrophic currents, tides, and inertial oscillations, which are estimated at about 5 cm s/sup -1/. Two rings in the Cape Basin and an intense vortex in the Argentine Basin exhibit significant centripetal contributions ! to the measured flow; when they are removed, the comparisons ! with geostrophy improve. Differences, or cross-track bottom currents, are significantly above noise only in the Argentine Basin; three regions are identified there. In the Falkland Current strong barotropic components (16 to 40 cm s/sup -1/ northward) augment the baroclinic transport fourfold to 50 Sv (Sv identical to 10/sup 6/ m/sup 3/ s/sup -1/), in accordance with the arguments of Peterson and the predictions of a numerical ocean model (FRAM). It follows that this will have a large impact on heat, salt, and tracer fluxes across the section, though these are not discussed. The second region of significant bottom flow is in the confluence zone (Brazil and Falkland Current Extension), where intense surface circulations penetrate in attenuated form (+12 to -18 cm s/sup -1/) to the seabed at 5000-m depth. Extremely turbid bottom mixed layers were detected there with transmittance values of 10% m/sup -1/, verifying the existence of strong currents. The third region of significa! nt bottom flows is contiguous with and east of the confluence zone, where a broad region of southerly flow is succeeded by a similar region of northerly flow (-15 to +8 cm s/sup -1/). These lie over a shallow abyssal ridge, with axis along the cruise track (the Zapiola Drift), which exhibited mud waves throughout and was draped with a turbid bottom layer. An anticyclonic flow about the Zapiola Drift has been inferred from the morphology of the mud waves seen on its flanks, and this circulation is shown to be contemporary by two current meter records from the region. Th authors' measurements appear to confirm this è ciulation and suggest that the strength exceeds 100 Sv. Is this a recirculation such as seen near the Gulf Stream extension? No evidence for it is found in numerical models and further observations of its existence are needed. The authors believe that the bottom currents over the deepest parts of the Argentine Basin are strong over a wide area. The value of combining the GPS3DF and ADCP observations in order to identify regions of strong bottom flows is demonstrated. DE: oceanographic-regions MN: J181-95004 AN: 5383247 *LHM: Connect to this title online; UW restricted http://ams.allenpress.com/amsonline/?request=get-archive&issn=1520-0485 See records of latest issues received http://catalog.lib.washington.edu/record=b2038065 Location: Available Online Location: Available Online -- Shelved by title: Full Text through ProQuest Direct http://proquest.umi.com/pqdlink?Ver=1&Exp=07-01-2003&REQ=3&Cert=7YMWy6YMy6bpLgoHt04CRpK0odiyGY8GFyPJRYCOyb4QcDP5iYc3XsCDREiVdG8Y&Pub=36166 -- LIB HAS: Jun.1998- -- Restricted to UW, and other Cooperative Library Project institutions. This title is purchased as part of the Cooperative Library Project. Location: Fish-Ocean Stacks -- Call number: GC1 .J68 -- LIB HAS: v.1- (1971-) -- Latest issues on display Record 5 of 26 in INSPEC 1996 TI: The Bernoulli function and flux of energy in the ocean AU: Saunders-PM SO: Journal-of-Geophysical-Research. vol.100, no.C11; 15 Nov. 1995; p.22647-8 PY: 1995 LA: English AB: Explains how the Bernoulli function, the total energy of a fluid, can be calculated from recent work on the thermodynamics of seawater. The Bernoulli function for an incompressible fluid has been used in the past to infer the absolute circulation of the ocean from hydrographic data alone. This is now both undesirable and unnecessary. Constructing the Bernoulli function for a hydrographic section also provides a rigorous procedure for calculating the total energy flux across the section, a quantity dominated by the "heat flux". DE: geophysical-fluid-dynamics; oceanography- AN: 5166137 *LHM: See records of latest issues received http://catalog.lib.washington.edu/record=b2037688 Location: null -- Call number: 538.705 TE Sec.C -- LIB HAS: v.83-104 (1978-1999) -- Sec.C (Oceans) Location: null -- Call number: 538.705 TE -- LIB HAS: v.64-v.82 (1959-1977) Location: Fish-Ocean Stacks -- Call number: 538.705 TE Sec.C -- LIB HAS: v.105- (2000-) -- Sec.C (Oceans); LATEST ISSUES ON DISPLAY Location: NatSci Periodicals -- Call number: 538.705 TE -- LIB HAS: v.54- (1949-) -- LATEST ISSUES ON DISPLAY Record 6 of 26 in INSPEC 1993-1994 TI: The flux of overflow water through the Charlie-Gibbs Fracture Zone AU: Saunders-PM SO: Journal-of-Geophysical-Research. vol.99, no.C6; 15 June 1994; p.12343-55 PY: 1994 LA: English AB: Reports the results of a set of measurements made within the Charlie-Gibbs Fracture Zone in 1988-1989. The principal data sources are year-long current meter records, 16 in number, and 23 conductivity-temperature-depth stations. The aim was to determine the flux of overflow water passing westward out of the Iceland Basin in the eastern North Atlantic. Within the fracture zone, overflow water is defined either as having salinity greater than 34.94 at the present time or, more generally, as having a potential density sigma /sub 0/>27.8 kg/m/sup 3/. In 1988-1989 the core salinity had a value equal to that reported in 1981 and 1983 but was fresher by about 0.02 than was found in 1964. The flux was estimated twice per day and was found to fluctuate strongly, with energy spread in a broad band of periods, ranging from 10 to 400 days. No annual signal could be detected. The mean value was 2.4+or-0.5 Sv, less than all previous estimates based on hydrography alone. It is suggest! ed that hydrography may systematically overestimate transport because diffusion is neglected. Flux estimates from current meter arrays are rarely used in initializing numerical ocean models; consequently measurements, like those reported, are an independent and important means for assessing the performance of such models. DE: oceanographic-regions AN: 4733480 *LHM: See records of latest issues received http://catalog.lib.washington.edu/record=b2037688 Location: null -- Call number: 538.705 TE Sec.C -- LIB HAS: v.83-104 (1978-1999) -- Sec.C (Oceans) Location: null -- Call number: 538.705 TE -- LIB HAS: v.64-v.82 (1959-1977) Location: Fish-Ocean Stacks -- Call number: 538.705 TE Sec.C -- LIB HAS: v.105- (2000-) -- Sec.C (Oceans); LATEST ISSUES ON DISPLAY Location: NatSci Periodicals -- Call number: 538.705 TE -- LIB HAS: v.54- (1949-) -- LATEST ISSUES ON DISPLAY Record 7 of 26 in INSPEC 1993-1994 TI: Transport, heat, and freshwater fluxes within a diagnostic numerical model (FRAM) AU: Saunders-PM; Thompson-SR SO: Journal-of-Physical-Oceanography. vol.23, no.3; March 1993; p.452-64 PY: 1993 LA: English AB: Results are presented from the integration of a fine-resolution numerical model of the ocean operating in a diagnostic mode. The region covered lies south of 24 degrees S, as depicted in the FRAM Atlas. Transports of heat, salt, and freshwater fluxes are examined at 60 degrees S and near 30 degrees S in all three oceans. The results are found to be generally realistic. At midlatitude the meridional heat flux is largely determined by the structure of the mean meridional motions and to a lesser degree by the gyre-scale horizontal motions. These roles are reversed for freshwater fluxes. At a fixed high latitude the freshwater flux is determined by the mean meridional motions and the heat flux principally by the large-scale wandering of the circumpolar current across the latitude. Only in this latter case, namely for the heat flux at 60 degrees S, do mesoscale motions contribute to a significant extent. The model underestimates the production and export of abyssal water; th! e climatological state with which it is initialized is identified as the likely cause. A suggestion is offered for assessing the accuracy of diagnostic integrations. DE: oceanographic-regions AN: 4526660 *LHM: Connect to this title online; UW restricted http://ams.allenpress.com/amsonline/?request=get-archive&issn=1520-0485 See records of latest issues received http://catalog.lib.washington.edu/record=b2038065 Location: Available Online Location: Available Online -- Shelved by title: Full Text through ProQuest Direct http://proquest.umi.com/pqdlink?Ver=1&Exp=07-01-2003&REQ=3&Cert=7YMWy6YMy6bpLgoHt04CRpK0odiyGY8GFyPJRYCOyb4QcDP5iYc3XsCDREiVdG8Y&Pub=36166 -- LIB HAS: Jun.1998- -- Restricted to UW, and other Cooperative Library Project institutions. This title is purchased as part of the Cooperative Library Project. Location: Fish-Ocean Stacks -- Call number: GC1 .J68 -- LIB HAS: v.1- (1971-) -- Latest issues on display Record 8 of 26 in INSPEC 1990-1992 TI: Combining hydrographic and shipborne ADCP measurements AU: Saunders-PM SO: Deep-Sea-Research,-Part-A-(Oceanographic-Research-Papers). vol.39, no.7A-8A; July-Aug. 1992; p.1417-27 PY: 1992 LA: English AB: Observations with a shipborne Acoustic Doppler Current Profiler (ADCP) were made in the Faeroe Bank Channel. When underway in strong winds and rough seas, spurious current (<50 cm s/sup -1/) were observed which vanished when the ship was heave to. On station strong tidal/inertial currents were detected (ca 20 cm s/sup -1/) at two locations, over periods of 12 and 27 h. Transient current estimates were extracted by a least-squares model fit and the residuals filtered by optimum interpolation. The resulting non-divergent currents were combined with geostrophic shear derived from simultaneous CTD and XBT observations. Transports of, and mixing within, the Norwegian Sea overflow confirm previous determinations. The implication of this research for the conduct of WOCE transoceanic sections is described. DE: oceanographic-regions; oceanographic-techniques AN: 4261199 *LHM: See records of latest issues received http://catalog.lib.washington.edu/record=b2048072 Location: Fish-Ocean Stacks -- Call number: GC1 .D2512 -- LIB HAS: v. 26-39 (1979-1992) Location: FriHarbor Periodicals -- Call number: GC1 .D2512 -- LIB HAS: v. 26-39 (1979-1992) Record 9 of 26 in INSPEC 1990-1992 TI: Communication, semiotics and the mediating role of the technical writer AU: Saunders-PM SO: IPCC 89. Communicating to the World. International Professional Communication Conference (Cat. No.89CH2786-2). IEEE, New York, NY, USA; 1989; xiv+286 pp. p.102-5 PY: 1989 LA: English AB: The author addresses the topic 'how computer manuals come to mean what they mean' from an interdisciplinary perspective. M.A.K. Halliday (1978) offers a useful analysis of three functions of language, ideational, interpersonal, and textual, and their corresponding situational elements of field, tenor, and mode. These reflect the semiotic nature of language. Field of discourse includes the activities and actions of users and contains a web of meanings into which both manual and documentation fall. reciprocity is achieved when both meet the 'mutuality of expectations' of users. Users derive meaning and contribute to it be virtue of their place within such cultural and situational contexts, and language use serves a symbolic boundary signifying community membership. The manual and the technology it represents enter into and cannot escape this cultural coding process, a process which shapes the perceptions of all who share the environment. Neither a detailed description of ! the tasks performed by a user nor the steps required to complete these tasks tell us anything about the social semiotic process which takes place in an office or factory. This presents a major challenge to usability testers. DE: economic-and-sociologic-effects; human-factors; technical-presentation; user-manuals AN: 3684785 *LHM: Local holdings could not be determined - Consult UW catalogs at http://catalog.lib.washington.edu/search~/ Record 10 of 26 in INSPEC 1990-1992 TI: Cold outflow from the Faroe Bank Channel AU: Saunders-PM SO: Journal-of-Physical-Oceanography. vol.20, no.1; Jan. 1990; p.29-43 PY: 1990 LA: English AB: The exchange of water between the Norwegian Sea and the North Atlantic around the Faroe Islands was investigated in 1987 and 1988 combining CTD data with shipborne acoustic Doppler current profiler (ADCP). DE: oceanographic-regions AN: 3620102 *LHM: Connect to this title online; UW restricted http://ams.allenpress.com/amsonline/?request=get-archive&issn=1520-0485 See records of latest issues received http://catalog.lib.washington.edu/record=b2038065 Location: Available Online Location: Available Online -- Shelved by title: Full Text through ProQuest Direct http://proquest.umi.com/pqdlink?Ver=1&Exp=07-01-2003&REQ=3&Cert=7YMWy6YMy6bpLgoHt04CRpK0odiyGY8GFyPJRYCOyb4QcDP5iYc3XsCDREiVdG8Y&Pub=36166 -- LIB HAS: Jun.1998- -- Restricted to UW, and other Cooperative Library Project institutions. This title is purchased as part of the Cooperative Library Project. Location: Fish-Ocean Stacks -- Call number: GC1 .J68 -- LIB HAS: v.1- (1971-) -- Latest issues on display Record 11 of 26 in INSPEC 1985-1989 TI: Bottom currents near a small hill on the Madeira Abyssal Plain AU: Saunders-PM SO: Journal-of-Physical-Oceanography. vol.18, no.6; June 1988; p.868-79 PY: 1988 LA: English AB: Near-bottom currents at depths in excess of 5000 m have been measured in the Great Meteor East study area (near 31 degrees 20'N, 25 degrees W) over a 3-year period. The sites selected were on top of a small abyssal hill, on its flank, and on the abyssal plain 30 km distant from the hill. The magnitude of the mean current 10 m above the seabed was 1-2 cm s/sup -1/ but its direction was quite different at the three sites and reflected the presence of a clockwise vortex trapped over the hill. On the plain the mean flow direction was to the west and directly opposed to that furnished by a beta -spinal analysis of the density field. It is suggested that time dependent variations in the large-scale density field are more important than hitherto supposed. DE: oceanography- AN: 3253508 *LHM: Connect to this title online; UW restricted http://ams.allenpress.com/amsonline/?request=get-archive&issn=1520-0485 See records of latest issues received http://catalog.lib.washington.edu/record=b2038065 Location: Available Online Location: Available Online -- Shelved by title: Full Text through ProQuest Direct http://proquest.umi.com/pqdlink?Ver=1&Exp=07-01-2003&REQ=3&Cert=7YMWy6YMy6bpLgoHt04CRpK0odiyGY8GFyPJRYCOyb4QcDP5iYc3XsCDREiVdG8Y&Pub=36166 -- LIB HAS: Jun.1998- -- Restricted to UW, and other Cooperative Library Project institutions. This title is purchased as part of the Cooperative Library Project. Location: Fish-Ocean Stacks -- Call number: GC1 .J68 -- LIB HAS: v.1- (1971-) -- Latest issues on display Record 12 of 26 in INSPEC 1985-1989 TI: Flow through Discovery Gap AU: Saunders-PM SO: Journal-of-Physical-Oceanography. vol.17, no.5; May 1987; p.631-43 PY: 1987 LA: English AB: A narrow gap (Discovery Gap) in the East Azores Fracture Zone at 37 degrees N in the eastern Atlantic provides a channel for the exchange of bottom water between the Madeira and Iberian abyssal basins. A detailed survey defines its length (150 km), width (10-50 km), depth of sills (near 4800 m) and sediment thickness (0-500 m). Year-long measurements of deep flow are made from six moorings and ten current meters. These data are supplemented by 10 days of float tracking near 4700 m and numerous density profiles within and around the gap. An estimate is derived for the diapycnal diffusivity. DE: oceanography- AN: 3015583 *LHM: Connect to this title online; UW restricted http://ams.allenpress.com/amsonline/?request=get-archive&issn=1520-0485 See records of latest issues received http://catalog.lib.washington.edu/record=b2038065 Location: Available Online Location: Available Online -- Shelved by title: Full Text through ProQuest Direct http://proquest.umi.com/pqdlink?Ver=1&Exp=07-01-2003&REQ=3&Cert=7YMWy6YMy6bpLgoHt04CRpK0odiyGY8GFyPJRYCOyb4QcDP5iYc3XsCDREiVdG8Y&Pub=36166 -- LIB HAS: Jun.1998- -- Restricted to UW, and other Cooperative Library Project institutions. This title is purchased as part of the Cooperative Library Project. Location: Fish-Ocean Stacks -- Call number: GC1 .J68 -- LIB HAS: v.1- (1971-) -- Latest issues on display Record 13 of 26 in INSPEC 1985-1989 TI: The accuracy of measurement of salinity, oxygen and temperature in the deep ocean AU: Saunders-PM SO: Journal-of-Physical-Oceanography. vol.16, no.1; Jan. 1986; p.189-95 PY: 1986 LA: English AB: Institute of Oceanographic Science (IOS) experiences comparing temperatures measured with reversing thermometers, CTD and current meters is described. With considerable care these laboratory calibrated instruments are shown to be capable of an absolute accuracy of a few millidegrees. It is proposed that carefully calibrated IOS moored instruments be used as comparison sites for other workers. Measurements of salinity made by different laboratories are compared and recommendations for the measurement of dissolved oxygen concentrations are put forward. DE: chemical-variables-measurement; oceanographic-equipment; temperature-measurement AN: 2673373 *LHM: Connect to this title online; UW restricted http://ams.allenpress.com/amsonline/?request=get-archive&issn=1520-0485 See records of latest issues received http://catalog.lib.washington.edu/record=b2038065 Location: Available Online Location: Available Online -- Shelved by title: Full Text through ProQuest Direct http://proquest.umi.com/pqdlink?Ver=1&Exp=07-01-2003&REQ=3&Cert=7YMWy6YMy6bpLgoHt04CRpK0odiyGY8GFyPJRYCOyb4QcDP5iYc3XsCDREiVdG8Y&Pub=36166 -- LIB HAS: Jun.1998- -- Restricted to UW, and other Cooperative Library Project institutions. This title is purchased as part of the Cooperative Library Project. Location: Fish-Ocean Stacks -- Call number: GC1 .J68 -- LIB HAS: v.1- (1971-) -- Latest issues on display Record 14 of 26 in INSPEC 1985-1989 TI: The search for hydrothermal sources on the Mid-Atlantic Ridge AU: Saunders-PM; Francis-TJG SO: Progress-in-Oceanography. vol.14; 1985; p.527-36 PY: 1985 LA: English AB: In a search for hydrothermal vents in the median valley of the Mid-Atlantic Ridge, twenty seven lowerings of a telemetering thermistor probe were made between 43 degrees and 47 degrees N. No hot spots were detected. Below 3000 m valleys were found filled with water of more-or-less uniform potential temperature indicating weak but efficient mixing. The mechanisms for the renewal of the mixed water and the control exercised by the sill on them is reviewed. Sill locations and depths are identified for seven valley segments in the study area. Sill depths range from 2100 to 2850 m. Within the valleys the temperature at a depth of 3000 m ranges from 3.56 to 3.17 degrees C, decreasing as the sill depth increases. A strategy is proposed for exploring a series of such valleys in a systematic search for the presence of hydrothermal vents employing chemical sampling of Mn, CH/sub 4/, or /sup 3/He. DE: geology-; groundwater-; oceanic-crust; oceanography-; terrestrial-heat AN: 2434481 *LHM: Connect to all available issues of this title online; UW restricted; http://www.sciencedirect.com/science/journal/00796611 See records of latest issues received http://catalog.lib.washington.edu/record=b1996119 Location: Available Online Location: Fish-Ocean Stacks -- Call number: 551.4605 PR -- LIB HAS: v.1- (1963-) -- LATEST ISSUES IN: DISPLAY Record 15 of 26 in INSPEC 1980-1984 TI: Benthic observations on the Madeira Abyssal Plain: currents and dispersion AU: Saunders-PM SO: Journal-of-Physical-Oceanography. vol.13, no.8; Aug. 1983; p.1416-29 PY: 1983 LA: English AB: An experiment to measure near-bottom currents on the Madeira Abyssal Plain is described. The moorings placed near 33 degrees N, 22 degrees W were separated by 5-40 km with instruments at 10, 100 and 600 m above the bottom (depth approximately 5300 m). The analysis separates currents into tidal, inertial and low frequency components. The M/sub 2/ tide is found to be principally barotropic with magnitude, ellipticity, orientation and phase adequately predicted by the tidal model of Schwiderski (1979). Oscillations of near-inertial frequency are found to be bottom intensified; their phase velocity is directed downward suggesting the bottom as the source. The vertical group velocity is estimated. Low-frequency statistics are presented also revealing bottom intensification. By assuming equality of Eulerian and Lagrangian time scales the author estimates the abyssal (horizontal) diffusivity. Spatial correlations are calculated for the array, and the transverse velocity functi! on is found to have a zero-crossing near 35 km. Streamfunction maps are made at 10-day intervals by the method of optimum linear interpolation. Trajectories are calculated over a 6-12 day period. Trajectories are calculated for the behavior of 170 pairs of particles at initial separations 1-20 km for up to 10 days. The merits and limitations of the methods employed are discussed. DE: oceanography- AN: 2200803 *LHM: Connect to this title online; UW restricted http://ams.allenpress.com/amsonline/?request=get-archive&issn=1520-0485 See records of latest issues received http://catalog.lib.washington.edu/record=b2038065 Location: Available Online Location: Available Online -- Shelved by title: Full Text through ProQuest Direct http://proquest.umi.com/pqdlink?Ver=1&Exp=07-01-2003&REQ=3&Cert=7YMWy6YMy6bpLgoHt04CRpK0odiyGY8GFyPJRYCOyb4QcDP5iYc3XsCDREiVdG8Y&Pub=36166 -- LIB HAS: Jun.1998- -- Restricted to UW, and other Cooperative Library Project institutions. This title is purchased as part of the Cooperative Library Project. Location: Fish-Ocean Stacks -- Call number: GC1 .J68 -- LIB HAS: v.1- (1971-) -- Latest issues on display Record 16 of 26 in INSPEC 1980-1984 TI: Abyssal temperature measurements with Aanderaa current meters AU: Saunders-PM; Cherriman-JW SO: Deep-Sea-Research,-Part-A-(Oceanographic-Research-Papers). vol.30, no.6A; June 1983; p.663-7 PY: 1983 LA: English AB: Modifications of the Aanderaa RCM5 current meter temperature circuit are described; a sensitivity of 2.5 mC degrees suitable for abyssal studies is achieved. Pre- and post-cruise calibrations of a group of instruments show remarkable stability and from the internal consistency of the records the absolute accuracy is estimated near 3 mC degrees . Comparisons with lowered CTD observations suggest that observing climatic changes of ocean temperature of 0.01 C degrees is a formidable task. DE: oceanographic-equipment; oceanography- AN: 2130481 *LHM: See records of latest issues received http://catalog.lib.washington.edu/record=b2048072 Location: Fish-Ocean Stacks -- Call number: GC1 .D2512 -- LIB HAS: v. 26-39 (1979-1992) Location: FriHarbor Periodicals -- Call number: GC1 .D2512 -- LIB HAS: v. 26-39 (1979-1992) Record 17 of 26 in INSPEC 1980-1984 TI: Subsurface circulation in the Somali Current AU: Leetmaa-A; Rossby-HT; Saunders-PM; Wilson-P SO: Science. vol.209, no.4456; 1 Aug. 1980; p.590-2 PY: 1980 LA: English AB: Direct velocity measurements were made at intermediate depths along the East African coast from March to July 1979. Strong time-dependent flows with multiple reversals in direction were found in the upper 1000 meters between 3 degrees N and 4 degrees S. At 700 meters, there may be a connection between the southwestward coastal current and an equatorial jet observed at 49 degrees E, the latter turning south near the coast. North of 3 degrees N little spatial organization of the flow can be recognized. DE: oceanography- AN: 1649212 *LHM: Connect to older issues of this title online; UW restricted; http://www.jstor.org/fcgi-bin/jstor/listjournal.fcg/00368075?config=jstor&frame=frame&userID=805f68d3@washington.edu/018dd5531e00503d353f&dpi=3 Connect to current issues of this title online; UW restricted http://www.sciencemag.org See records of latest issues received http://catalog.lib.washington.edu/record=b2028877 Location: null -- Call number: 505 S -- LIB HAS: n.s. v.207-286 (1980-1999) Location: Available Online Location: Available Online Location: Available Online -- Shelved by title: Full Text through ProQuest Direct http://proquest.umi.com/pqdlink?Ver=1&Exp=07-01-2003&REQ=3&Cert=7YMWy6YMy6bpLgoHt04CRpK0odiyGY8GFyPJRYCOyb4QcDP5iYc3XsCDREiVdG8Y&Pub=28298 -- LIB HAS: Jan.1988-Aug/1999 -- Restricted to UW, and other Cooperative Library Project institutions. This title is purchased as part of the Cooperative Library Project. Location: Available Online -- Shelved by title: Some articles are available from Lexis-Nexis online. http://www.lib.washington.edu/databases/LexisNexis/catlink.html -- UW Restricted Location: Bothell/CCC Microforms -- Call number: Microfilm BOT-41 -- LIB HAS: v.227- (1985-) Location: Bothell/CCC Periodicals -- Shelved by title: Science -- Call number: Q1 .S352 -- Current issues only; Held until microfilm received. Location: Chem Periodicals -- Call number: 505 S -- LIB HAS: n.s. v.175-286 (1972-1999) Location: Engr Periodicals-Floor 2 -- Shelved by title: Science -- Call number: 505 S -- LIB HAS: n.s. v.231-286 no.5449 (1986-1999) -- Incomplete v.241 Location: Fish-Ocean Stacks -- Call number: 505 S -- LIB HAS: n.s. v.287- (2000-) -- LATEST ISSUES ON DISPLAY Location: FriHarbor Periodicals -- Shelved by title: Science -- Call number: 505 S -- LIB HAS: n.s. v.23- (1906-) Location: Health Serials -- Shelved by title: Science -- Call number: 505 S -- LIB HAS: v.1(1883)-v.14(1889), v.24(1906)-v.279(1998) v.280:n.5360-5366,5368-5372(1998:Apr 3-May 15,May 29-Jun 26) v.281(1998)-v.286(1999) -- Pre-1930 vols. in Basement Storage Location: KKSherwood Lib-Harborview -- Shelved by title: Science -- Call number: Per -- LIB HAS: v.247(1990)-v.290(2000) Location: NatSci Periodicals -- Call number: 505 S -- LIB HAS: v.1-23; n.s. v.1- (1883-) -- LATEST ISSUES IN nscir; LIBRARY USE ONLY Location: Odegaard Per - Micro -- Shelved by title: Science -- Call number: Microfilm B1432 -- LIB HAS: n.s. v.202- (1978-) -- LIBRARY USE ONLY Location: Odegaard Periodicals -- Shelved by title: Science -- Call number: 505 S -- LATEST ISSUES ON DISPLAY; Held until microfilm received; LIBRARY USE ONLY Location: Phys-Astr Periodicals -- Shelved by title: Science -- Call number: 505 S -- Latest 2 years only; issues are kept on display; LIBRARY USE ONLY Location: Tacoma Microforms -- Call number: Microfilm TAC-41 -- LIB HAS: v.227-286 (1985-1999) Location: Tacoma Periodicals -- Call number: Q1 .S352 -- Current issues only; Held until microfilm received Location: Auxiliary Stacks -- Call number: 505 S -- LIB HAS: n.s. v.119-230 (1954-1985) -- Incomplete v.123, 127, 140, 142 Record 18 of 26 in INSPEC 1969-1979 TI: Tests on flux distortion flowmeters using an analogue rig to simulate flow with a boundary layer AU: Baker-RC; Saunders-PM SO: Annals-of-Nuclear-Energy. vol.4, no.9-10; 1977; p.457-64 PY: 1977 LA: English AB: A rig for testing the behaviour of flux distortion flowmeters is described which makes use of moving brass tubes instead of flowing sodium. The tubes simulate the flow and by moving concentric tubes at different speeds a stepped 'boundary layer' is simulated. The results obtained from this rig are given and the likely errors are discussed. The comparison with earlier numerical prediction programs is satisfactory. DE: boundary-layers; fission-reactor-core-control-and-monitoring; flowmeters-; nuclear-reactor-instrumentation; simulation- AN: 1187174 *LHM: See records of latest issues received http://catalog.lib.washington.edu/record=b2017650 Location: Engr Periodicals-Floor 2 -- Shelved by title: Annals of nuclear energy -- Call number: QC770 .A523 -- LIB HAS: v.2-24, v.25 no.7, v.26 no.1, no.2, & no.4 (1975-May 1998) Record 19 of 26 in INSPEC 1969-1979 TI: Wind stress on the ocean over the eastern continental shelf of North America AU: Saunders-PM SO: Journal-of-Physical-Oceanography. vol.7, no.4; July 1977; p.555-66 PY: 1977 LA: English AB: Employing one million ship reports gathered in the years 1941-72 seasonal averages of the wind stress and its standard deviation have been computed for the shelf region of the eastern North American continent (out to a depth of 200 m). A drag coefficient is assumed which increases with wind speed. Atmospheric stratification is taken into account but its effect is shown to be small. DE: oceanography-; wind- AN: 1128869 *LHM: Connect to this title online; UW restricted http://ams.allenpress.com/amsonline/?request=get-archive&issn=1520-0485 See records of latest issues received http://catalog.lib.washington.edu/record=b2038065 Location: Available Online Location: Available Online -- Shelved by title: Full Text through ProQuest Direct http://proquest.umi.com/pqdlink?Ver=1&Exp=07-01-2003&REQ=3&Cert=7YMWy6YMy6bpLgoHt04CRpK0odiyGY8GFyPJRYCOyb4QcDP5iYc3XsCDREiVdG8Y&Pub=36166 -- LIB HAS: Jun.1998- -- Restricted to UW, and other Cooperative Library Project institutions. This title is purchased as part of the Cooperative Library Project. Location: Fish-Ocean Stacks -- Call number: GC1 .J68 -- LIB HAS: v.1- (1971-) -- Latest issues on display Record 20 of 26 in INSPEC 1969-1979 TI: Average drag in an oscillatory flow AU: Saunders-PM SO: Deep-Sea-Research. vol.24, no.4; April 1977; p.381-4 PY: 1977 LA: English AB: In an oscillatory flow u with nonzero mean it is shown that the time averaged drag on an obstacle (or the bottom) can be approximated by the expression rho Ca omega u where a omega is the amplitude of the oscillatory component. This result is valid for a omega >or= mod u mod . This can be applied to the estimation of the drag exerted on a moored surface buoy, on a drogued buoy and on a fixed or towed surface structure in ocean currents or waves. DE: liquid-oscillations; oceanography- AN: 1087603 *LHM: See records of latest issues received http://catalog.lib.washington.edu/record=b2050337 Location: Fish-Ocean Stacks -- Call number: GC1 .D25 -- LIB HAS: v. 1-8. (Oct. 1953-1961.) Location: FriHarbor Periodicals -- Call number: GC1 .D25 -- LIB HAS: v. 1-8. (Oct. 1953-1961.) Record 21 of 26 in INSPEC 1969-1979 TI: Near-surface current measurements AU: Saunders-PM SO: Deep-Sea-Research. vol.23, no.3; March 1976; p.249-57 PY: 1976 LA: English AB: Near-surface current measurements made in the JASIN '72 (Joint Air-Sea Interaction) experiment have been intercompared. There is close agreement between the measurements of a 10-m VACM (Vector averaging current meter) under a toroid moored in 2500 m of water and of 12-m drifters tracked from a ship: differences were only 2 cm s/sup -1/ in currents ranging from 10 to 30 cm s/sup -1/. Comparisons of the 10-m VACM and a 12-m Aanderaa meter revealed that the Aanderaa vane failed to follow the frequency reversals associated with the surface gravity wave field and hence the instrument biased currents high (by factors of between 1 and 10). A model demonstrated this failing; it is suggested that VACM measurements also bias high (by 10%) but no sure evidence could be found. DE: oceanographic-equipment; oceanographic-techniques AN: 915519 *LHM: See records of latest issues received http://catalog.lib.washington.edu/record=b2050337 Location: Fish-Ocean Stacks -- Call number: GC1 .D25 -- LIB HAS: v. 1-8. (Oct. 1953-1961.) Location: FriHarbor Periodicals -- Call number: GC1 .D25 -- LIB HAS: v. 1-8. (Oct. 1953-1961.) Record 22 of 26 in INSPEC 1969-1979 TI: The instability of a baroclinic vortex AU: Saunders-PM SO: Journal-of-Physical-Oceanography. vol.3, no.1; Jan. 1973; p.61-5 PY: 1973 LA: English AB: An experimental study is made of a baroclinic vortex produced in a two-layer fluid. After the equivalence between the experiment and the heated annulus experiment of Hide (1971) is established, it is argued that the potential energy of the stratification is the source for wave-like instabilities which develop and split the vortex into separate, distinct circulations. The stability of some mesoscale oceanic vortices is examined. DE: liquid-waves; oceanography-; rotational-flow; stability-; vortices- AN: 532685 *LHM: Connect to this title online; UW restricted http://ams.allenpress.com/amsonline/?request=get-archive&issn=1520-0485 See records of latest issues received http://catalog.lib.washington.edu/record=b2038065 Location: Available Online Location: Available Online -- Shelved by title: Full Text through ProQuest Direct http://proquest.umi.com/pqdlink?Ver=1&Exp=07-01-2003&REQ=3&Cert=7YMWy6YMy6bpLgoHt04CRpK0odiyGY8GFyPJRYCOyb4QcDP5iYc3XsCDREiVdG8Y&Pub=36166 -- LIB HAS: Jun.1998- -- Restricted to UW, and other Cooperative Library Project institutions. This title is purchased as part of the Cooperative Library Project. Location: Fish-Ocean Stacks -- Call number: GC1 .J68 -- LIB HAS: v.1- (1971-) -- Latest issues on display Record 23 of 26 in INSPEC 1969-1979 TI: Space and time variability of temperature in the upper ocean AU: Saunders-PM SO: Deep-Sea-Research. vol.19, no.7; July 1972; p.467-80 PY: 1972 LA: English AB: Five flights were made during a three-week period in the spring of 1968 over an area of side 200 km in the Ionian Sea. Observations were made of the surface temperature employing an infra-red radiometer, and calibration checks and environmental corrections ensured high quality data. Comparison with ship records shows the radiometer measurements had an accuracy of +or-0.2 degrees C. A detail hydrographic survey of the region was made concurrently with the aircraft programme and the connection between surface flow and the temperature field established from maps produced by objective analysis. Regions of surface currents were revealed by horizontal variability in temperature and marked by advective events; stagnant regions showed horizontal uniformity of temperature and steady seasonal warming. A statistical analysis was made of the temperature data and over the range of scales 3-100 km the density of temperature variance E/sub T/(k) was shown to obey a law E/sub T/(k) app! roximately k/sup -p/, where k is the wavenumber and p=2.2+or-0.1. This power law does not fit any proposed model of geophysical turbulence. DE: oceanography-; temperature-distribution AN: 442208 *LHM: See records of latest issues received http://catalog.lib.washington.edu/record=b2050337 Location: Fish-Ocean Stacks -- Call number: GC1 .D25 -- LIB HAS: v. 1-8. (Oct. 1953-1961.) Location: FriHarbor Periodicals -- Call number: GC1 .D25 -- LIB HAS: v. 1-8. (Oct. 1953-1961.) Record 24 of 26 in INSPEC 1969-1979 TI: Comments on 'wavenumber-frequency spectra of temperature in the free atmosphere' (with authors reply) AU: Saunders-PM; Kao-S-K SO: Journal-of-the-Atmospheric-Sciences. vol.29, no.1; Jan. 1972; p.197-201 PY: 1972 LA: English AB: For original article see ibid., vol. 27, 1007 of 1970. DE: atmospheric-temperature AN: 400849 *LHM: Connect to this title online; UW restricted http://ams.allenpress.com/amsonline/?request=get-archive&issn=1520-0469 See records of latest issues received http://catalog.lib.washington.edu/record=b2037756 Location: Available Online Location: Available Online -- Shelved by title: Full Text through ProQuest Direct http://proquest.umi.com/pqdlink?Ver=1&Exp=07-01-2003&REQ=3&Cert=7YMWy6YMy6bpLgoHt04CRpK0odiyGY8GFyPJRYCOyb4QcDP5iYc3XsCDREiVdG8Y&Pub=11543 -- LIB HAS: Aug.1997- -- Restricted to UW, and other Cooperative Library Project institutions. This title is purchased as part of the Cooperative Library Project. Location: Fish-Ocean Stacks -- Call number: QC851 .J74 -- LIB HAS: v.1-54 (Sept. 1944-1997) Location: NatSci Periodicals -- Call number: 551.505 JO -- LIB HAS: v.1- (Sept. 1944-) -- LATEST ISSUES ON DISPLAY Record 25 of 26 in INSPEC 1969-1979 TI: Anticyclonic eddies formed from shoreward meanders of the Gulf Stream AU: Saunders-PM SO: Deep-Sea-Research. vol.18, no.12; Dec. 1971; p.1207-19 PY: 1971 LA: English AB: During a 3-month period (September to December, 1969) measurements with an airborne radiation thermometer and air-dropped BT's revealed the existence of a northward meander of the Gulf Stream, its amplification and the production of an anticyclonic eddy (diameter ca. 100 km). In the same area and period (October to December, 1968) 60 days of current records were obtained at six depths from the surface down to 2000 m; they show that the meander and eddy circulations are confined to the upper 1000 m and are weak with surface currents of only 30-75 cm/sec. The energy of the eddy is shown to reside principally in the form of available potential energy, which is present in the local deformation of the density field and estimated to be 10/sup 23/ ergs; this quantity is 30 times larger than the total kinetic energy of the circulation (3*10/sup 21/ ergs). Estimates are made of the rate of destruction of the total energy of the eddy by (i) enhanced heat loss to the atmosphere an! d (ii) dissipation of kinetic energy by turbulent vertical diffusion: the eddy lifetime from these processes is estimated as 6 months and 1 year respectively. DE: oceanography- AN: 388975 *LHM: See records of latest issues received http://catalog.lib.washington.edu/record=b2050337 Location: Fish-Ocean Stacks -- Call number: GC1 .D25 -- LIB HAS: v. 1-8. (Oct. 1953-1961.) Location: FriHarbor Periodicals -- Call number: GC1 .D25 -- LIB HAS: v. 1-8. (Oct. 1953-1961.) Record 26 of 26 in INSPEC 1969-1979 TI: Corrections for airborne radiation thermometry AU: Saunders-PM SO: Journal-of-Geophysical-Research. vol.75, no.36; 20 Dec. 1970; p.7596-601 PY: 1970 LA: English AB: The PRT5 was used for the remote measurement of ocean surface temperature. The correction for nonblackness of the ocean ranges from +0.6 degrees C (under clear skies) to +0.1 degrees C (under a low overcast). From an altitude of 300 meters the correction for absorption and emission in the intervening atmosphere can be approximated by 0.1 (T-T/sub A/), where T is the indicated radiometric temperature and T/sub A/ is the air temperature at flight level. The influence of haze is investigated experimentally and found to be small. Absolute accuracy of the measurements when made carefully from low altitude is +or-0.2 degrees C. DE: oceanography- AN: 242423 *LHM: See records of latest issues received http://catalog.lib.washington.edu/record=b2037688 Location: null -- Call number: 538.705 TE Sec.C -- LIB HAS: v.83-104 (1978-1999) -- Sec.C (Oceans) Location: null -- Call number: 538.705 TE -- LIB HAS: v.64-v.82 (1959-1977) Location: Fish-Ocean Stacks -- Call number: 538.705 TE Sec.C -- LIB HAS: v.105- (2000-) -- Sec.C (Oceans); LATEST ISSUES ON DISPLAY Location: NatSci Periodicals -- Call number: 538.705 TE -- LIB HAS: v.54- (1949-) -- LATEST ISSUES ON DISPLAY