1. Remote GPS Networks: Rationale
Carol A. Raymond, Erik R. Ivins
JPL/Caltech

2. Rationale for Antarctic Continuous GPS stations and Constraints on Station Architecture
Continuous GPS measurements contribute to understanding the interaction between ice sheet history and dynamics, and earth rheology. Support time-varying gravity measurements of ice mass change.
Rationale for Continuous Measurements:
Vertical rates are low (typically few cm?) and need for accuracy is high to resolve gentle gradients
Incomplete noise characterization (phase center drifts, biases, seasonal tropospheric variations, ionosphere, reference frame issues)for data lengths of < 30 days?
Constraints:
If rheology is stiff, and loads are ancient, uplift gradients are small
If loads are young, uplift gradients might be large.
Likely there will be a spectrum of uplift scales that must be deconvolved to understand their origin in lateral heterogeneity of earth rheology, and/or glacial loading histories of individual drainage basins

3. High precision vertical components are critical for distinguishing competing models
Current results favor recent ice mass change - indicating smaller scale gradients are expected

4. Proposed TAM CGPS Network continues decadal-length times series at 4 sites
WAGN
occupations
W13
Network proposed in 2004 (Raymond et al.) is designed to measure glacioisostatic deformation in region most sensitive to testing models
Donnellan and Luyendyk ( )
Raymond et al. ( )
TAMDEF
Air Force Seismic Stations (new)

5. Proposed Next-Generation Station Architecture

6. Picosat and UAV System Engineering (PAUSE)
Li-SoCl2 batteries
Magnetometer package is undergoing lab thermal testing (30 C to -60C)
Stratospheric balloon tests in October 2004
Components, software and architecture can be reused for GPS stations
Freewave
modem
magnetometer
single board
computer

7. Tumbleweed Polar Rover