Synthesis of enantiopure cyclopentanones by desymmetrization of allylic cyclobutanols

The interest in five-membered ring molecules derives from their important application in many different fields, such as pharmaceutical and agrochemical areas. A common strategy for their formation is four-membered ring expansion, which also allows to add molecular complexity and functional handles within one single operation starting from readily available starting materials. Organocatalysis can be exploited to promote the reaction and to obtain a good enantio- and diastereoselection. This technique involves the exclusive use of organic molecules as catalysts, without resorting to metals. The aim of this work is to obtain enantiopure cyclopentanones starting from achiral allylic cyclobutanols. The reaction consists in a ring expansion promoted by the addition of a halogen to the double bond of the substrate, with formation of a haliranium ion as intermediate, followed by a semipinacol rearrangement to afford the cyclopentanone. The reaction is catalysed by a chiral phosphoric acid that, besides accelerating the rate of the reaction, transmits a specific chirality thanks to its chiral structure, following the asymmetric catalysis principles. Starting from symmetric trans-allylic cyclobutanols, the whole reaction is a desymmetrization and leads to the formation of two new stereogenic centres: a mixture of diastereoisomers is obtained, each as couple of enantiomers; the ratio between the possible configurations is determined by the relative position that the chiral catalyst and the reagent occupy during the reaction. Since the reaction is already optimized, the original aim was to study the scope: first, the synthesis of a set of allylic cyclobutanols and their relative precursors, in order to have a wider range of substrates; then, the identification of the type of substrate that undergoes the expansion, with the study of enantio- and diastereoselectivity obtained in each case. Due to the Covid-19 emergency, most of the work was developed as a bibliographic study.

Characterization of ENSO changes under idealised radiative forcing in an intermediate complexity general circulation model

Intermediate-complexity general circulation models are a fundamental tool to investigate the role of internal and external variability within the general circulation of the atmosphere and ocean. The model used in this thesis is an intermediate complexity atmospheric general circulation model (SPEEDY) coupled to a state-of-the-art modelling framework for the ocean (NEMO). We assess to which extent the model allows a realistic simulation of the most prominent natural mode of variability at interannual time scales: El-Niño Southern Oscillation (ENSO). To a good approximation, the model represents the ENSO-induced Sea Surface Temperature (SST) pattern in the equatorial Pacific, despite a cold tongue-like bias. The model underestimates (overestimates) the typical ENSO spatial variability during the winter (summer) seasons. The mid-latitude response to ENSO reveals that the typical poleward stationary Rossby wave train is reasonably well represented. The spectral decomposition of ENSO features a spectrum that lacks periodicity at high frequencies and is overly periodic at interannual timescales. We then implemented an idealised transient mean state change in the SPEEDY model. A warmer climate is simulated by an alteration of the parametrized radiative fluxes that corresponds to doubled carbon dioxide absorptivity. Results indicate that the globally averaged surface air temperature increases of 0.76 K. Regionally, the induced signal on the SST field features a significant warming over the central-western Pacific and an El-Niño-like warming in the subtropics. In general, the model features a weakening of the tropical Walker circulation and a poleward expansion of the local Hadley cell. This response is also detected in a poleward rearrangement of the tropical convective rainfall pattern. The model setting that has been here implemented provides a valid theoretical support for future studies on climate sensitivity and forced modes of variability under mean state changes.