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

(a) Time history of the shear rate of zonal flow ∂_xV_ZF(t) near the resonant surface (x = 0, ±2ρ_i, ±5ρ_i). Inset: shear profiles of zonal flow ∂_xV_ZF(x) at different time.