- Page 1 and 2:
1Oth International
- Page 3:
Preface It is truly a great pleasur
- Page 6 and 7:
Speaker: Dan Cooley................
- Page 8 and 9:
Speaker: Qian Li ..................
- Page 10 and 11:
Speaker: Ediang Okuku Archibong....
- Page 12 and 13:
Speaker: Yi Wang...................
- Page 14 and 15:
Climatological Dataset.............
- Page 16 and 17:
Bridging the gap between simulated
- Page 18 and 19:
Invited Session: Spatial patterns o
- Page 20 and 21:
Joint Program on the Science and Po
- Page 22 and 23:
e to adopt a different calibrated l
- Page 24 and 25:
those retained, and [iii] performan
- Page 26 and 27:
A range of existing statistical app
- Page 28 and 29:
palaeo-environmental data from sout
- Page 30 and 31:
Whilst it has been noted that such
- Page 32 and 33:
State Key Laboratory of Numerical M
- Page 34 and 35:
address new policies for changing c
- Page 36 and 37:
and show promise for analyzing tren
- Page 38 and 39:
1901-2005 with complete data of all
- Page 40 and 41:
Homogenization of daily meteorologi
- Page 42 and 43:
as Homogen Data, Gap, Index, Statis
- Page 44 and 45:
Penalized maximal t-test for detect
- Page 46 and 47:
Iran,Tehran, Azad university, Resea
- Page 48 and 49:
We present applications of several
- Page 50 and 51:
A 50-member ensemble is produced wi
- Page 52 and 53:
ichard@stats.ucl.ac.uk Nadja Leith
- Page 54 and 55: Answering questions about empirical
- Page 56 and 57: In a series of climate change impac
- Page 58 and 59: climatological annual frequency of
- Page 60 and 61: Detection of urban warming in recen
- Page 62 and 63: Detection of Human Influence on pan
- Page 64 and 65: Extending attribution studies: post
- Page 66 and 67: Francis W. Zwiers, Gabriele C. Hege
- Page 68 and 69: 1, In the middle-pattern of El Niñ
- Page 70 and 71: convergence zone (ITCZ). Th
- Page 72 and 73: stationary waves occur in mid-latit
- Page 74 and 75: A multiple surrogate data study of
- Page 76 and 77: Linear and non-linear reconstructio
- Page 78 and 79: Pseudo-proxy tests of the regulariz
- Page 80 and 81: Parallel Sessions:Regional Studies
- Page 82 and 83: Iterative Interpolation of Daily Pr
- Page 84 and 85: disturbance in the natural ecosyste
- Page 86 and 87: Climate Risk Management in North-Ea
- Page 88 and 89: Analyzing of synoptic intence showe
- Page 90 and 91: chosen since it completely defines
- Page 92 and 93: The Roles of Ensem
- Page 94 and 95: The diagram shows
- Page 96 and 97: Empirical probabilistic seasonal fo
- Page 98 and 99: Rajesh J. Department of Atmospheric
- Page 100 and 101: Andrew Moore Uni. of California at
- Page 102 and 103: Parallel Sessions:Simulation tools
- Page 106 and 107: egion can be explained by the rando
- Page 108 and 109: on instantaneous time scales, respe
- Page 110 and 111: Key words:- principal component reg
- Page 112 and 113: een analysed with geostatistical to
- Page 114 and 115: Iberian Peninsula and with the corr
- Page 116 and 117: 89% during the 10 days of mid-June,
- Page 118 and 119: The paper examines
- Page 120 and 121: Special AMS Session:Verification of
- Page 122 and 123: Verification of Climate Forecasts (
- Page 124 and 125: the regional climate change is repr
- Page 126 and 127: model has been applied to the serie
- Page 128 and 129: are analyzed. It is shown that thes
- Page 130 and 131: stations in Iran. The</stro
- Page 132 and 133: The study of the U
- Page 134 and 135: Development and analysis of a daily
- Page 136 and 137: Fractal widely exists in nature, an
- Page 138 and 139: Rescue of historical climate data:
- Page 140 and 141: D. Semeradova Institute of Landscap
- Page 142 and 143: Kulkarni Ashwini, Sabade S S and Kr
- Page 144 and 145: The magnitude of t
- Page 146 and 147: Richard E. Chandler University Coll
- Page 148 and 149: convective cloud clusters when they
- Page 150 and 151: 1999; Smith et al, 2001; Gibbons, 2
- Page 152 and 153: dmanatsa@buse.ac.zw Wisemen Chingom
- Page 154 and 155:
The Relation Betwe
- Page 156 and 157:
conditioned on some indices of the
- Page 158 and 159:
ari@ludens.elte.hu J. Bartholy Dept
- Page 160 and 161:
ainfall as predictand. Additionally
- Page 162 and 163:
Impact of ENSO PHASES on Amazonia S
- Page 164 and 165:
time lag. Both perturbed analysis a
- Page 166 and 167:
Relationship Between Ensemble Mean
- Page 168 and 169:
ways were considered. Four zones, f
- Page 170 and 171:
- Monthly ratios of synthetic and o
- Page 172 and 173:
Total ozone trends are typically st
- Page 174 and 175:
Impact of Urban Expansion on Region
- Page 176 and 177:
Calibrating and evaluating reanalys
- Page 178:
To explore an optimal climate decis