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) Odd and (b) even parities of the absolute value of the ITG modes | ϕ∼ | with k_yρ_i = 0.5 at t = 0.8 × 10⁴ (before transition) and t = 1.2 × 10⁴ (after transition). (c) Shear of the zonal flow profile ∂_xV_ZF at t = 0.8 × 10⁴ (during transition).