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Anne F. Dallmeyer Max-Planck-Institut für Meteorologie Bundesstrasse 53 20146 Hamburg Germany Als Dissertation angenommen vom Department Geowissenschaften der Universität Hamburg auf Grund der Gutachten von Prof. Dr. Martin Claussen und Dr. Victor Brovkin Hamburg, den 2. November 2011 Prof. Dr. Jürgen Oßenbrügge Leiter des Departments für Geowissenschaften ISSN 1614-1199
Holocene climate and vegetation change in the Asian monsoon region Anne F. Dallmeyer Hamburg 2011
Page 1: Holocene climate and vegetation cha
Page 6 and 7: Overleaf Sutlej Valley, Kalpa (31°
Page 8 and 9: Zusammenfassung Mittels verschieden
Page 10 and 11: II 3.5 Summary and conclusion of Ch
Page 12 and 13: List of Figures Figure 2.1: Simulat
Page 14 and 15: Figure 4.7: Simulated differences i
Page 16 and 17: Figure A.1: The Asian monsoon regio
Page 19 and 20: 1. Introduction Like all monsoon sy
Page 21 and 22: (I) How well is the present-day Asi
Page 23 and 24: CHAPTER 5 The Tibetan Plateau exert
Page 25 and 26: 2. Simulated present-day Asian mons
Page 27 and 28: In this study, we assess the perfor
Page 29 and 30: in the local summer season. This la
Page 31 and 32: Figure 2.2: Hovmöller diagram show
Page 33 and 34: 2.3.2 Monsoon onset and withdrawal
Page 35 and 36: to observations and reanalysis data
Page 37 and 38: and as indices the method of prescr
Page 39 and 40: investigated by comparing atmospher
Page 41 and 42: T 3 1 _ A _ A M I P [ °C ] T 6 3 _
Page 43 and 44: - Overall, the simulation T31AV0k a
Page 45 and 46: 3. Simulated mid-Holocene Asian mon
Page 47 and 48: Values were taken from a course res
Page 49 and 50: To further analyse the differences
Page 51 and 52: Figure 3.6: Simulated difference in
Page 53 and 54: Figure 3.8: Annual cycle of precipi
Page 55 and 56:
in these regions during the pre-mon
Page 57 and 58:
positive anomaly (more divergent) i
Page 59 and 60:
our results, we compare the reconst
Page 61 and 62:
Figure 3.15: Differences in the sea
Page 63 and 64:
mid-Holocene climate north of 40°N
Page 65 and 66:
4. Contribution of the atmosphere-o
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includes the dynamic vegetation mod
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Region Approximate longitude (°E)
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Figure 4.2: Seasonal and annual ave
Page 73 and 74:
Figure 4.3: Same as Figure 4.2, but
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nearby desert or sparsely vegetated
Page 77 and 78:
Figure 4.5: Factors contributing to
Page 79 and 80:
spring summer autumn winter spring
Page 81 and 82:
In autumn, the contribution of the
Page 83 and 84:
Figure 4.8: Same as Figure 4.5 but
Page 85 and 86:
The atmospheric response to the orb
Page 87 and 88:
Due to the thermal inertia of the o
Page 89 and 90:
eduction of -0.97K (on average) is
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climate in 6k. Whether the ocean-at
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econstructions (Yu et al., 2000). T
Page 95 and 96:
5. Comparison of the simulated Holo
Page 97 and 98:
ased vegetation reconstructions for
Page 99 and 100:
(Zhang et al. 2000; Fang et al. 200
Page 101 and 102:
Figure 5.2: ECHAM5 orography (eleva
Page 103 and 104:
unfavourable climate conditions, i.
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vegetation type exists and the land
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etreat and were replaced by steppes
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exceeds 4000m in reality (cf. Fig.
Page 111 and 112:
5.5.2 Site-specific discussion of t
Page 113 and 114:
Figure 5.7: Change of the climate f
Page 115 and 116:
Figure 5.8: Simulated change of sum
Page 117 and 118:
Overall, the simulated forest fract
Page 119 and 120:
simulated climate for SETP strongly
Page 121 and 122:
6. Sensitivity of the Asian monsoon
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6.5k. Afterwards, land cover gradua
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additionally accounted for. The soi
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total grass sum per grid-box is sca
Page 129 and 130:
In the dry/cold season, the strong
Page 131 and 132:
6.4.1 Change of circulation and wat
Page 133 and 134:
Figure 6.7: Simulated change of dif
Page 135 and 136:
6.4.2 Change of albedo and turbulen
Page 137 and 138:
In the dry/cold season, deforestati
Page 139 and 140:
Figure 6.13: Simulated change in mo
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Northeast China (increase), regardl
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a.) Local effect: - The impact of l
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7. Summary and Conclusion 7.1 Summa
Page 147 and 148:
strongest temperature change in the
Page 149 and 150:
suggested in previous paleo-reconst
Page 151 and 152:
Bibliography Adler, R.F., Huffman,
Page 153 and 154:
Claussen, M.: Late Quaternary veget
Page 155 and 156:
Gasse, F., Arnold, M., Fontes, J.Ch
Page 157 and 158:
Joussaume, S., and Braconnot, P.: S
Page 159 and 160:
Marsland, S. J., Haak, H., Jungclau
Page 161 and 162:
Roeckner, E., Brokopf, R., Esch, M.
Page 163 and 164:
Ueno, K., Fujii, H., Yamada, H., an
Page 165 and 166:
Wu, G.X., Wang, J., Liu, X., and Li
Page 167 and 168:
Appendix A: Additional figures A.I
Page 169 and 170:
Figure A.4: Sketch of the main mean
Page 171 and 172:
Figure A.7: Same as Figure A.6, but
Page 173 and 174:
Appendix B: Additional tables B.I S
Page 175 and 176:
Appendix C: Summary of the simulate
Page 177 and 178:
Figure C.4: Same as Figure C.1, but
Page 179 and 180:
Figure C.7: Same as Figure C.5, but
Page 181 and 182:
Acknowledgements I would like to ac
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