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As a consequence, the earthflow hazard maps representing the probability of temporal occurrence of the failures for the critical rainfall threshold value of 107.5 mm in the
Johns, “Asymptotic distribution of linear combinations of functions of order statistics with applications to estimation,” Annals of Mathematical Statistics, vol.. Hosking,
Aydi, “Common fixed point results for mappings satisfying ψ, φ-weak contractions in ordered partial metric spaces,” International Journal of Mathematics and Statistics, vol..
Cathy Macharis, Department of Mathematics, Operational Research, Statistics and Information for Systems (MOSI), Transport and Logistics Research Group, Management School,
On the other hand, the classical theory of sums of independent random variables can be generalized into a branch of Markov process theory where a group structure replaces addition:
We show (Theorem 4.2) that this interpretation extends to a q-analogue based on the statistic des for alternating Baxter permutations and number of cycles for genus zero per-
In particular, Section 4.1 deals with multiple Poisson integrals, Section 4.2 with de Jong’s theorem for degenerate U-statistics and Section 4.3 with non-degenerate U-statistics
In particular, we find that, asymptotically, the expected number of blocks of size t of a k-divisible non-crossing partition of nk elements chosen uniformly at random is (k+1)