Ocean Science Station

 

The Project
Research Methods
Research Questions
The Locations
How to Use This Site
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Part 1:
January 25 - February 9, 2005
The Team
Daily Journal

New Horizon Daily Report
New Horizon Cruise Track

Part 2:
July 23 - August 13, 2005
The Team
Daily Journal

New Horizon Daily Report

New Horizon Cruise Track

Part 3:
August 30 - September 8, 2005
The Team
Daily Journal

R/V Wecoma Daily Report
R/V Wecoma Cruise Track

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Daily Journal

Part 2
July 23 - August 13, 2005

23 July, 2005:












Today I’m writing for Eileen Purcell, who is feeling a bit under the weather. We left San Diego this morning under cloudy skies and with cool breezes. We will enjoy the refreshing weather while we can. Before we left the air conditioners were taken apart and put in good order. The extreme heat will stress both the ship’s electronics and our very precious water supply.

The rocking of the ship takes some getting used to the first day, even for some of the seasoned science veterans. Learning to stand and walk easily on a moving surface will be difficult until we all get our ‘sea legs.’ Ever notice, perhaps in a movie, that a boat in the ocean can be rocking with no wind at all? The rolling motions of the ocean, or swells, are caused by winds traveling across the ocean. This long-distance wind is called fetch. Local winds are what cause the tiny ripples and whitecaps on the surface of the swells.  –Ida Royer

Q: What are some ways the weather of other countries and far-away places can affect where you live?