A treatise on frequency spectrum of drift ice velocity
スポンサーリンク
概要
- 論文の詳細を見る
Sea ice dynamics is examined for the frequency spectra of ice velocity using mathematical models and ice motion data. The data are from the Baltic Sea and Sea of Okhotsk. A general spectrum for linear coupled ice-ocean free drift is derived and analysed. Interior dynamics shows singularity in the Coriolis (inertial) frequency and asymptotic high frequency power law of -2. In the presence of internal friction the spectrum is expected to evenly fall to zero with frictional resistance increasing above yield level. In the observations, the main spectral peak is wide at the synoptic time scales. The Okhotsk Sea spectra show inertial and tidal signals but they are missing from the Baltic Sea due to very weak tides and shallow depth damping inertial oscillations. Above semidiurnal frequency ice velocity spectra fall in power law of -5/3, inherited from atmospheric and oceanic dynamics, and at very high frequencies, above 0.5 cph the fall seems to slow down to power law below -1. The Eulerian ice velocity spectrum was higher than the Lagrangian spectrum throughout the entire obtained spectrum (0.1-5 cpd). Theoretical spectra show general agreement with observations except that they have less kinetic energy at very high frequencies and much stronger inertial peak. Thus Eulerian observations are more variable than Lagrangian observations.
論文 | ランダム
- 付録1 原子炉等利用に関する共同研究報告書
- 原子炉施設の放射線管理設備の更新と使用前検査結果
- 近畿大学原子炉とともに歩む ―核実験からJCO事故まで―
- 化石海水の同定法の提案 : 太平洋炭鉱における地下水水質・同位体分布と地下水年代評価
- 中性子回折によるアモルファス合金の構造観察