Basic features of the multiscale interaction between tearing modes and slab ion-temperature-gradient modes<xref rid="cpb_28_12_125203_fn1" ref-type="fn">*</xref><fn id="cpb_28_12_125203_fn1"><label>*</label><p>Project supported by the National Key R&D Program of China (Grant Nos. 2017YFE0301100 and 2017YFE0300500), the National Natural Science Foundation of China (Grant Nos. 11675038, 11775069, and 11305027), and the Fundamental Research Funds for the Central Universities of China (Grant No. DUT17RC(4)54).</p></fn>

Basic features of the multiscale interaction between tearing modes and slab ion-temperature-gradient modes**

Project supported by the National Key R&D Program of China (Grant Nos. 2017YFE0301100 and 2017YFE0300500), the National Natural Science Foundation of China (Grant Nos. 11675038, 11775069, and 11305027), and the Fundamental Research Funds for the Central Universities of China (Grant No. DUT17RC(4)54).

Wei L^{1, †}, Wang Z X^{1, ‡}, Li J Q², Hu Z Q¹, Kishimoto Y³

Snapshots of the velocity fluctuations in the x-direction v∼x (top row) and b∼xv∼∥ (bottom row) during the transition phase. The contour lines of the magnetic flux near the resonant surface represent the magnetic field lines or corresponding magnetic island. In this case, the resistivity is set to η = 1.1 × 10⁻⁴.