SCICEX Hydrographic Data, 1997 and 1998 Introduction: The Scientific Ice Expeditions (SCICEX) Program is a series of scientific field operations within the Arctic Ocean using US Navy operational submarines as sampling platforms. The 1997 SCICEX cruise aboard the USS Archerfish was the third in the series, and the 1998 SCICEX cruise aboard the USS Hawkbill was the fourth. The project is multi-disciplinary in nature with a broad range of measurement goals held by the multiple PI's. The overarching goal is to characterize the upper layers of the sampled regions of the Arctic Ocean as completely as possible. The measurements described here sampled the upper 800m of the ocean with submarine launched conductivity, temperature and depth probes. Data Acquisition and Processing: The profile data were collected using Sippican model 306700-1 Under-Ice Submarine-Launched Expendable Conductivity, Temperature and Depth probes. These probes are launched from the submerged submarine, rise under their own buoyancy to a depth of about 15 m, then release from their buoyant components and free-fall. Profiles are measured during the free-fall period while the probes remain connected to the shipboard datalogger via signal cables. Probe depths are computed based on a known fall rate, temperature (T) and conductivity values are measured by probe sensors and returned as functions of depth, and salinity (S) is computed from these values. The design accuracy of the probes is 0.02 degrees C in T, 0.05 practical salinity units (psu) in S and 5 m in depth except for the uppermost 5 m of the record (15-20 m depths), where data are unreliable during equilibration of the probe sensors and are typically discarded. Data collection software was Sippican MK12 for Windows, version 1.3. Subsequent processing was completed with MATLAB (www.mathworks.com) running under Windows NT, using the SEAWATER library, a collection of oceanographic functions in the MATLAB language developed by the Commonwealth Scientific and Industrial Research Organisation (CSIRO) in Hobart, Australia. Derived variables include pressure (in db, calculated from depth and latitude), potential temperature (in degrees C), sigma-t (a representation of density in kg/m^3), and sigma-theta (sigma-t calculated with potential temperature). Data Set Coverage: The 1997 profiles were collected from just north of Fram Strait along a transect to the Alaskan Coast, westward along the shelf break to the Laptev Sea and back into the interior of the basin, crisscrossing the Canadian basin and eventually ending near the Bering Strait. Distance between profiles was variable. Profile data were generally collected to a depth of 1000 m at 1-m intervals in the vertical. Data were collected between September 3 and October 2, 1997. The data are available in ASCII text format along with the accompanying documentation in Microsoft Word format in the zip file scicex97_xctd.zip. The 1998 profiles were collected along a transect following the shelf break in the Chuckchi Sea, crossing the Arctic Ocean into the interior of the Nansen Basin then crossing the Amunsen Basin to the eastern terminus of the Lomonosov Ridge. The cruise track then extended into the Makarov and Canada Basins and over the Chuckchi Cap. Distance between profiles was variable. Profile data were generally collected to a depth of 1000 m at 1-m intervals. Data were collected between August 1 and September 2, 1998. The data are available in ASCII text format along with the accompanying documentation in Microsoft Word format in the zip file scicex98_xctd.zip. An online interactive map, powered by Environmental Systems Research Institute's (ESRI's) ArcIMS version 3.1, is available on the product Web site. The map displays the spatial distribution of data collection points, and may be used to select profiles of interest and to view data. Contacts and Acknowledgments: PI: Robin D. Muench Earth & Space Research Data Contact: John T. Gunn Earth & Space Research ONR Grant: N00014-96-1-0855