Figures & data
Table 1. Physical and mechanical parameters of rock and joint.
Figure 2. (a) Time-history acceleration of different ground motions and (b) corresponding Fourier spectrum.
![Figure 2. (a) Time-history acceleration of different ground motions and (b) corresponding Fourier spectrum.](/cms/asset/283b3227-b14f-4980-88b9-317dc88d4fb1/tgnh_a_2301532_f0002_c.jpg)
Table 2. Numerical simulation models and the corresponding parameters.
Figure 3. Effect of normalized stiffness K on spatial variation of AAF-X of the slope: (a) K=0.5, (b) K=1, (c) K=10, and (d) homogeneous slope.
![Figure 3. Effect of normalized stiffness K on spatial variation of AAF-X of the slope: (a) K=0.5, (b) K=1, (c) K=10, and (d) homogeneous slope.](/cms/asset/cef61379-acf7-4af7-98d5-abd265e984e3/tgnh_a_2301532_f0003_b.jpg)
Figure 4. (a) The AAF-X along the slope surface with different normalized stiffness K and (b) the AAF-X at the slope crest and for different distances behind the slope crest.
![Figure 4. (a) The AAF-X along the slope surface with different normalized stiffness K and (b) the AAF-X at the slope crest and for different distances behind the slope crest.](/cms/asset/8964c30a-56e6-4269-bcce-94b2270e08de/tgnh_a_2301532_f0004_c.jpg)
Figure 5. Effect of kn/ks on spatial variation of AAF-X of the slope: (a) kn/ks = 1, (b) kn/ks = 6, and (c) kn/ks = 10.
![Figure 5. Effect of kn/ks on spatial variation of AAF-X of the slope: (a) kn/ks = 1, (b) kn/ks = 6, and (c) kn/ks = 10.](/cms/asset/4858d4ee-443d-4551-a072-11f600662cde/tgnh_a_2301532_f0005_b.jpg)
Figure 6. (a) The AAF-X along the slope surface with different kn/ks and (b) the AAF-X at the slope crest and for different distances behind the slope crest.
![Figure 6. (a) The AAF-X along the slope surface with different kn/ks and (b) the AAF-X at the slope crest and for different distances behind the slope crest.](/cms/asset/a659b808-bd75-43c7-9a4b-b1accb25317e/tgnh_a_2301532_f0006_c.jpg)
Figure 7. Effect of normalized joint spacing ξ on spatial variation of AAF-X of the slope: (a) ξ = 0.005, (b) ξ = 0.01, and (c) ξ = 0.1.
![Figure 7. Effect of normalized joint spacing ξ on spatial variation of AAF-X of the slope: (a) ξ = 0.005, (b) ξ = 0.01, and (c) ξ = 0.1.](/cms/asset/bff57982-92ed-46fc-a127-84347e085644/tgnh_a_2301532_f0007_b.jpg)
Figure 8. (a) The AAF-X along the slope surface with different normalized joint spacing ξ and (b) the AAF-X at the slope crest and for different distances behind the slope crest.
![Figure 8. (a) The AAF-X along the slope surface with different normalized joint spacing ξ and (b) the AAF-X at the slope crest and for different distances behind the slope crest.](/cms/asset/9717d30d-7b78-4604-8b84-e3de28aa8637/tgnh_a_2301532_f0008_c.jpg)
Figure 9. Effect of slope angle i on spatial variation of AAF-X of the slope: (a) i = 15°, (b) i = 30°, (c) i = 45°, (d) i = 60°, (e) i = 75°and (f) i = 90°.
![Figure 9. Effect of slope angle i on spatial variation of AAF-X of the slope: (a) i = 15°, (b) i = 30°, (c) i = 45°, (d) i = 60°, (e) i = 75°and (f) i = 90°.](/cms/asset/04fb5b72-4820-4296-945e-fef40d302072/tgnh_a_2301532_f0009_b.jpg)
Figure 10. (a) The AAF-X along the slope surface for jointed slope with different slope angle i, (b) the AAF-X along the slope surface for homogeneous slope with different slope angle i, and (c) the AAF-X at the slope crest for jointed and homogeneous slope.
![Figure 10. (a) The AAF-X along the slope surface for jointed slope with different slope angle i, (b) the AAF-X along the slope surface for homogeneous slope with different slope angle i, and (c) the AAF-X at the slope crest for jointed and homogeneous slope.](/cms/asset/d9c27c2a-74d9-41f2-812f-5c2bdd9d2bd1/tgnh_a_2301532_f0010_c.jpg)
Figure 11. (a) The AAF-X along the slope surface for jointed slope with different slope height H, (b) the AAF-X along the slope surface for homogeneous slope with different slope height H, and (c) the AAF-X at the slope crest with different H/λ by varying the slope height.
![Figure 11. (a) The AAF-X along the slope surface for jointed slope with different slope height H, (b) the AAF-X along the slope surface for homogeneous slope with different slope height H, and (c) the AAF-X at the slope crest with different H/λ by varying the slope height.](/cms/asset/5aad4970-84cb-4baa-adfa-e8e488d210db/tgnh_a_2301532_f0011_c.jpg)
Figure 12. Seismogram synthetics of acceleration for different K: (a) K = 0.5, (b) K = 1, (c) K = 3, and (d) K = 10.
![Figure 12. Seismogram synthetics of acceleration for different K: (a) K = 0.5, (b) K = 1, (c) K = 3, and (d) K = 10.](/cms/asset/47beb903-391d-4cec-9ee3-06b8b7a5859e/tgnh_a_2301532_f0012_c.jpg)
Figure 13. Seismogram synthetics of acceleration for different ξ: (a) ξ=0.005, (b) ξ=0.01, (c) ξ=0.02, and (d) ξ=0.1.
![Figure 13. Seismogram synthetics of acceleration for different ξ: (a) ξ=0.005, (b) ξ=0.01, (c) ξ=0.02, and (d) ξ=0.1.](/cms/asset/304724e1-bc2f-4fa3-b433-1a75933a49bd/tgnh_a_2301532_f0013_c.jpg)
Figure 14. The topographic and jointed amplification function: (a) TAtopo_ho of the homogeneous model, (b) TAtopo_jo of the jointed model, (c) TAsite for 1D and 2D models, and (d) TAcoupled.
![Figure 14. The topographic and jointed amplification function: (a) TAtopo_ho of the homogeneous model, (b) TAtopo_jo of the jointed model, (c) TAsite for 1D and 2D models, and (d) TAcoupled.](/cms/asset/0b9abe7a-4397-43cc-83b1-8ce2b22a1d76/tgnh_a_2301532_f0014_c.jpg)
Table 3. Recorded PGAs at the free surface of the 1D soil column and 2D slope models.
Figure 15. Seismogram synthetics of acceleration for different slope heights. Left (homogeneous slope): (a) H=30m, (b) H=90m, (c) H=300m, and (d) H=900m; Right (jointed slope): (e) H=30m, (f) H=90m, (g) H=300m, and (h) H=900m.
![Figure 15. Seismogram synthetics of acceleration for different slope heights. Left (homogeneous slope): (a) H=30m, (b) H=90m, (c) H=300m, and (d) H=900m; Right (jointed slope): (e) H=30m, (f) H=90m, (g) H=300m, and (h) H=900m.](/cms/asset/6ccd85e6-b780-4cde-a7b0-37dee1aad28f/tgnh_a_2301532_f0015_c.jpg)
Data availability statement
The datasets generated and analyzed during the current study are available from the corresponding author on reasonable request.