9.5.2 Evidence from the benthosIn a time series of observations on cha terjemahan - 9.5.2 Evidence from the benthosIn a time series of observations on cha Bahasa Indonesia Bagaimana mengatakan

9.5.2 Evidence from the benthosIn a

9.5.2 Evidence from the benthos
In a time series of observations on changes in the biomass, abundance, and species
number in the subtidal benthos at a site off the German coast of the southern North
Sea, Kroncke et al. (1998) found clear correlations between the properties of the
benthos in the summer and the NAO index of the preceding winter. The authors
had previously ruled out changes in sediment composition, coastal morphology,hot summers, or storm events as important factors in the changes in the benthos.
It seemed that mild winters associated with a strongly positive NAO were conducive
to increases in the benthos. Particularly large changes in the benthos occurred
in 1989 and 1990, reinforcing the idea that this was a period of regime change in
the North Sea.
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9.5.2 Evidence from the benthosIn a time series of observations on changes in the biomass, abundance, and speciesnumber in the subtidal benthos at a site off the German coast of the southern NorthSea, Kroncke et al. (1998) found clear correlations between the properties of thebenthos in the summer and the NAO index of the preceding winter. The authorshad previously ruled out changes in sediment composition, coastal morphology,hot summers, or storm events as important factors in the changes in the benthos.It seemed that mild winters associated with a strongly positive NAO were conduciveto increases in the benthos. Particularly large changes in the benthos occurredin 1989 and 1990, reinforcing the idea that this was a period of regime change inthe North Sea.
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9.5.2 Bukti dari bentos
Dalam serangkaian waktu pengamatan pada perubahan biomassa, kelimpahan, dan spesies
nomor di bentos subtidal di sebuah situs di lepas pantai Jerman bagian selatan North
Sea, Kroncke et al. (1998) menemukan korelasi yang jelas antara sifat-sifat
benthos di musim panas dan indeks NAO dari musim dingin sebelumnya. Para penulis
sebelumnya telah mengesampingkan perubahan komposisi sedimen, morfologi pantai, musim panas yang panas, atau peristiwa badai sebagai faktor penting dalam perubahan benthos.
Tampaknya musim dingin ringan terkait dengan NAO sangat positif kondusif
untuk peningkatan benthos. Khususnya perubahan besar dalam benthos terjadi
pada tahun 1989 dan 1990, memperkuat gagasan bahwa ini adalah masa perubahan rezim di
Laut Utara.
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