This article mainly informative, some ways of algebraic modeling of human genome sequences is presented, with special emphasis on describing mutations in the genes, which by modifying proteinsynthesis involve genetic diseases such as Diabetes Mellitus. Mutations as endomorphisms on an R-module, which consists of a direct sum of groups of sequences 2q37.3 gene, on the rings Z64 and Z125, where el haplotype compound for the polymorphisms SNP43, SNP19 and SNP63 occur.

We describe a model that interprets the circulation of the tropical ocean in the periods when the meteorological phenomenon known as "El Niño" appears; A study area is defined as being the equatorial pacific, the ocean current is described by the primitive equations, which consists of the equations of motion and temperature transport which are strongly coupled. As boundary conditions, the wind stresses on the surface of the ocean is fundamental for the warming of waters, which due to its high variability we consider it random and described by a multiplicative white noise, generating the so-called stochastic primitive equations for the circulation of the tropical ocean.The variational formulation of the problem is presented and some estimates that allow verifying the existence of solutions of these equations.

This article mainly informative, some ways of algebraic modeling of human genome sequences is presented, with special emphasis on describing mutations in the genes, which by modifying proteinsynthesis involve genetic diseases such as Diabetes Mellitus. Mutations as endomorphisms on an R-module, which consists of a direct sum of groups of sequences 2q37.3 gene, on the rings Z64 and Z125, where el haplotype compound for the polymorphisms SNP43, SNP19 and SNP63 occur.

We describe a model that interprets the circulation of the tropical ocean in the periods when the meteorological phenomenon known as "El Niño" appears; A study area is defined as being the equatorial pacific, the ocean current is described by the primitive equations, which consists of the equations of motion and temperature transport which are strongly coupled. As boundary conditions, the wind stresses on the surface of the ocean is fundamental for the warming of waters, which due to its high variability we consider it random and described by a multiplicative white noise, generating the so-called stochastic primitive equations for the circulation of the tropical ocean.The variational formulation of the problem is presented and some estimates that allow verifying the existence of solutions of these equations.