Letter - E.C. Schmon to Arthur A. Schmon, 14 February 1918

The letter discusses Valentine's Day and she has drawn hearts in red ink. She also describes the events of the previous day: Red Cross work, lunch at YWCA, Club meeting. The letter also includes a list of items in a package she has sent to Arthur. The letter is labelled number 56.

Letter - E.C. Schmon to Arthur A. Schmon, 14 June 1918

Eleanore Celeste has been to visit Arthur Schmon's parents. His father has not been feeling well and takes a week vacation per month. His mother worries because the checks Arthur sends do not come when they should. Eleanore Celeste requests that Arthur write to Washington to have it straightened out. She also mentions her family and who they are visiting over the next week. This letter is labelled number 114.

Letter - E.C. Schmon to Arthur A. Schmon, 14 February 1920

This letter is decorated for Valentine's Day. There is a red cut out hard included that reads "To my Valentine from your Valentine xxxxxx". The second part of the letter talks about how to get to Shelter Bay and Eleanore Celeste remarks "So you do not think it advisable for me to make the trip to Shelter Bay by dog team! Let me tell you dearest, that I wouldn't mind if I had to walk there." These letters are labelled number 126 and 127.

Letter - E.C. Schmon to Arthur A. Schmon, 14 & 15 May 1919

Eleanore Celeste mentions that Arthur is to return in July. She discusses the way the troops are returning to New York and New Jersey and the discharge process. These letters are labelled number 279 and 280.

Letter - E.C. Schmon to Arthur A. Schmon, 14 March 1917

The letter is a thank you for a book Arthur has sent to Eleanore Celeste. The title of the book is not mentioned.

Modeling of atmospheric effects on InSAR measurements by incorporating terrain elevation information

We propose an elevation-dependent calibratory method to correct for the water vapour-induced delays over Mt. Etna that affect the interferometric syntheric aperture radar (InSAR) results. Water vapour delay fields are modelled from individual zenith delay estimates on a network of continuous GPS receivers. These are interpolated using simple kriging with varying local means over two domains, above and below 2 km in altitude. Test results with data from a meteorological station and 14 continuous GPS stations over Mt. Etna show that a reduction of the mean phase delay field of about 27% is achieved after the model is applied to a 35-day interferogram. (C) 2006 Elsevier Ltd. All rights reserved.