GEOS 597e
Spatiotemporal Data Analysis Workshop

Prework 3:  Know your data

This week we'll have our first look at the data we are going to use to study empirical orthogonal function analysis, and we'll estimate the temporal autocovariance of sea surface temperature anomaly by calculating the temporal covariance matrix of the gridded dataset.

Last updated 9/13/06.  To be completed prior to class session Weds., Sept. 13th.



Introduction:

Since the mid-19th century, volunteer observing ships and research vessels have made and reported observations of marine meteorological and atmospheric variables.  In the 1980s and 1990s, the Global Ocean Surface Temperature Atlas (GOSTA) project produced from this 'raw' data a gridded dataset for use in climatological studies.  This was -- and is -- not an easy task, for the heterogeneous nature of the dataset makes corrections for known and suspected random and systematic error difficult to know precisely.  Nevertheless, many of us in the climate research community would like to use this dataset to address a variety of important research questions.  Over the next several weeks we will analyze gridded sea surface temperature anomalies, a dataset known as British Meteorological Office Historical Sea Surface Temperatures (MOHSST5).

Reading:
Reading questions:
Products to hand in:
  1. In 1-2 paragraphs, please concisely write down your scientific question and list of uncertainties.  Be prepared to discuss in class whether you think this dataset is sufficient for the study of the scientific question you have in mind, given its inherent uncertainties.
  2. Your equation for the covariance of x and y.  Also, please answer the question: why is c an estimate of the true covariance C between X and Y?


Back to Schedule/Syllabus.