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1.5.1 Comparability of research methods
Different research scientists have used different methodologies depending on the parameters being investigated. Most researchers have used comparable methods. However, there are some methods that are not so comparable.
For example, in measuring waves, Lwiza1987 and Edet 1991 used graduated wave staffs. In cases like these, the results are rather subjective and hard to compare simply because the wave heights are observed visually, a
method that has high degree of uncertainty.
1.5.2 Sampling frequency and duration of studies
Sampling frequency has been varied depending on the type of study. In some studies, like those applying General Circulation Models, Computer and Mathematical are used. In this case there is no sampling frequency involved.
The same is true for the review studies. In some studies sampling frequency is not stated completely e.g. Edet, 1991. The sampling frequency available in many studies varied from half hourly measurements e.g. Hravey,
1977 to monthly measurements e.g. Mwaiseje, 1973. Others followed monsoon seasons e.g. Newell, 1957, 1959; Dubi and Nyandwi, 1999.
The duration of many studies has not been long enough to warrant long-term evaluations. For example, in the investigation of heavy mineral content of Tanzanian beach sands, Cilek 1976 took approximately one year to
conduct that study. But since heavy mineral composition is dependent on hydrodynamic conditions, the study is only good for baseline purposes. The situation could change after say, 20 years. This is the same situation for most
other studies.
1.5.3 Capability of researchers
Highly qualified scientists have carried out most of the studies. Even in cases where research has been done by students, supervision has been done by capable scientists and most of works have led to postgraduate degrees e.g.
Edet, 1991; Nzali, 1998.
1.5.4 Age of information
Information, which is older than 20 years, is considered old and its reliability is questionable. An exception to this fact is of course on geological studies. An overview of the status of some selected studies is summarised in Table
1.2.
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Table 1.2: Example of the sampling frequency and duration of some studies, where P indicates published articles and G is grey literature. The age of information is classified as either old or recent.
Article Duratio
n of studies
Sampling frequency Publication
Age of informa
tion Cilek 1976
1 year -
P Old
Cooke 1974. 1 year
- P
Old Dubi 1998
25 years Monthly maximum values
P Recent
Dubi and Nyandwi
1999 1 year
Tides, Currents : monthly.
Waves : every two-month.
Profiles and Sediment : neap
and spring tides P
Recent
Edet 1991 2 years
- MSc. Thesis
Recent Harvey 1977
20 years offshore
data
4 years Zanzibar
Channel
3 months at
Kunduch i
Half hourly for a period of 25 hours
Positions of drogues taken at 45 min. intervals.
Temperature, turbidity and water sample taken at 2 hours
interval P
Old
Kaaya and Boenigk
1986 1 year
- P
Old Mwaipopo
1984 2 years
Computer sampling P
Old Mwaiseje
1973 1 year
Monthly P
Old Nieuwolt
1973 4 years
3-hourly intervals P
Old Nzali et al.
1998 1 year
Every two-months for recruitment rates
four times a month for temperature and transparency
once every 4 – 5 days for sedimentation rates
P Recent
Shayo 1979 -
Computer sampling P
Old Temple and
Sundborg 1972
7 years data
Gage continuous? sampling P
Old
1.6 Main findingsobservations