vations from each of p genes. In [1] it is assumed that i , j = arg max{|β̂ij |} can be computed in time O(1) (it is also assumed that the inner products for updating the β̂ values can be computed in time O(1), but this is actually possible by using the fact that 〈Yk T , Y ∗ i − ηβ̂ijYj〉 = 〈Yk T , Y ∗ I 〉 − ηβ̂ij〈Yk T , Yi〉). This makes some sense, as the algorithm is implemented in Matlab and buil...

It has been shown that the static spin susceptibility of the Hubbard model of correlations for a narrow band calculated in the CPA remains finite for any simple-band model and the carrier number, except possibly in the case of a precisely half filled band. We show that this statement is more general and should be true if the Hubbard model could be solved exactly within the alloy analogy approxi...

The ability of 42 global climate models from the Coupled Model Intercomparison Project Phase 6 (CMIP6), consisting 20 low resolution (LR) and 22 medium (MR), are evaluated for their performance in simulating mean extreme precipitation over Indonesia. Compared to Climate Hazards Group InfraRed Precipitation with Station data (CHIRPS), model climatologies interannual variability investigated indi...

Hidden Markov Model on First Order Differences for Automatic Detection of Nucleosome Positions” Pei Fen Kuan1, Dana Huebert2, Audrey Gasch3, Sündüz Keleş1,4∗ 1Department of Statistics, University of Wisconsin, Madison, WI 53706. 2Department of Cellular and Molecular Biology, University of Wisconsin, Madison, WI 53706. 3Department of Genetics, University of Wisconsin, Madison, WI 53706. 4Departm...

[1] In a future climate warmed by increased greenhouse gases, increases of precipitation intensity do not have a uniform spatial distribution. Here we analyze a multi-model AOGCM data set to examine processes that produce the geographic pattern of these precipitation intensity changes over land. In the tropics, general increases in water vapor associated with positive SST anomalies in the warme...