Advanced representation of the ocean/sea ice dynamics at high latitudes

Sea ice is a fundamental element of global climate system, with numerous impacts on the polar environment. The ongoing drastic changes in the Earth’s sea ice cover highlight the necessity of monitoring the polar regions and systematically evaluating the quality of different numerical products. The main objective of this thesis is to improve our knowledge of the representation of Arctic and Antarctic sea ice using comprehensive global ocean reanalyses and coupled climate models. The dissertation will explore (i) the Antarctic marginal ice zone (MIZ) and pack ice area in the ensemble mean of four global ocean reanalyses called GREP; (ii) historical representation of the Arctic and Antarctic sea ice state in HighResMIP models; (iii) the future evolution of Arctic sea ice in HighResMIP models. Global ocean reanalyses and GREP are found to adequately capture interannual and seasonal variability in both pack ice and MIZ areas at hemispheric and regional scales. The advantage of the ensemble-mean approach is proved as GREP smooths the strengths and weaknesses of single systems and provides the most consistent and reliable estimates. This work is intended to encourage the use of GREP in a wide range of applications. The analysis of sea ice representation in the coupled climate models shows no systematic impact of the increased horizontal resolution. We argue that a few minor improvements in sea ice representation with the enhanced horizontal resolution are presumably not worth the major effort of costly computations. The thesis highlights the critical importance to distinguish the MIZ from consolidated pack ice both for investigating changes in sea ice distribution and evaluating the product’s performance. Considering that the MIZ is predicted to dominate the Arctic sea ice cover, the model physics parameterizations and sea ice rheology might require modifications. The results of the work can be useful for modelling community.

Analisi integrata di dati SAR e mareografici per lo studio dell’evoluzione di grandi masse di ghiaccio nell’ambito dei cambiamenti climatici: il caso del ghiacciaio Harald Moltke (Groenlandia).

Il progetto di tesi, inserito nel contesto degli studi sugli effetti dei cambiamenti climatici, si basa sull’utilizzo di dati radar derivanti dalla piattaforma satellitare Sentinel-1 (missione spaziale dell’Agenzia Spaziale Europea, inserita all’interno del progetto Copernicus) e mareografici, e ha l’obiettivo di verificare (e quindi validare) l’affidabilità dei dati Sentinel-1 per il monitoraggio della velocità e delle dinamiche di scioglimento del ghiacciaio Harald Moltke (Groenlandia) e la relazione con i fenomeni di distaccamento del suo fronte (eventi di “ice-calving”). Il monitoraggio del ghiacciaio e lo studio di questi ultimi eventi sono tra le tematiche legate al cambiamento climatico toccate dal progetto MACMAP (“A Multidisciplinary Analysis of Climate change indicators in the Mediterranean And Polar regions”, PI. A. Guarnieri, INGV) finanziate dell’istituto Nazionale di Geofisica e Vulcanologia. Per ottenere i campi di velocità del ghiacciaio sono stati utilizzati due dataset di immagini satellitari SAR (Sentinel-1) e, questi, elaborati con tecnica Offset tracking: il primo elaborato dal programma PROMICE e il secondo processato appositamente per questo lavoro con il tool SNAP (SentiNel Applications Platform, tool opensource creato dall’Agenzia Spaziale Europea, ESA). Per relazionare i fenomeni di calving con l’andamento della velocità del ghiacciaio sono stati integrati dati mareografici forniti dall’istituto INGV.

Chemical characterization by GC-MS and phytotoxic potential of non-polar and polar fractions of seeds of Dioteryx odorata (Aubl.) Willd. from Venezuelan regions

Dipteryx odorata (Aubl.) Willd. is a tall arboreal species native to Central and Northern South America. This paper describes the chemical characterization and phytotoxic potential of polar and non-polar extracts from D. odorata seeds. Structural determinations were accomplished by chemical derivatization and analyzed by GC/MS. The chemical composition of the non-polar fraction (hexane and dichloromethane) presented fatty acids as major constituent. Medium polar and polar fractions (ethyl acetate and ethanol: water) contained carboxylic acid and high 6,7-Dyhidroxycoumarin-β-D-glucopyranoside content, not previously reported for seeds of D. odorata. Extracts showed a significant level of phytotoxic activity, correlated to the content of coumarin derivatives, predominantly in the polar fraction.

Extended cusp-like regions and their dependence on the Polar orbit, seasonal variations, and interplanetary conditions

Extended cusp-like regions (ECRs) are surveyed, as observed by the Magnetospheric Ion Composition Sensor (MICS) of the Charge and Mass Magnetospheric Ion Composition Experiment (CAMMICE) instrument aboard Polar between 1996 and 1999. The first of these ECR events was observed on 29 May 1996, an event widely discussed in the literature and initially thought to be caused by tail lobe reconnection due to the coinciding prolonged interval of strong northward IMF. ECRs are characterized here by intense fluxes of magnetosheath-like ions in the energy-per-charge range of _1 to 10 keV e_1. We investigate the concurrence of ECRs with intervals of prolonged (lasting longer than 1 and 3 hours) orientations of the IMF vector and high solar wind dynamic pressure (PSW). Also investigated is the opposite concurrence, i.e., of the IMF and high PSW with ECRs. (Note that these surveys are asking distinctly different questions.) The former survey indicates that ECRs have no overall preference for any orientation of the IMF. However, the latter survey reveals that during northward IMF, particularly when accompanied by high PSW, ECRs are more likely. We also test for orbital and seasonal effects revealing that Polar has to be in a particular region to observe ECRs and that they occur more frequently around late spring. These results indicate that ECRs have three distinct causes and so can relate to extended intervals in (1) the cusp on open field lines, (2) the magnetosheath, and (3) the magnetopause indentation at the cusp, with the latter allowing magnetosheath plasma to approach close to the Earth without entering the magnetosphere.

Narrative of discovery and adventure in the polar seas and regions : with illustrations of their climate, geology, and natural history, and an account of the whale-fishery /

Publisher's advertisement: p. [1-18] at end.

Narrative of the recent voyage of Captain Ross to the Arctic regions, in the years 1829-30-31-32-33 : and a notice of Captain Back's expedition; with a preliminary sketch of polar discoveries, from the earliest period to the year 1827.

The preliminary sketch comp. chiefly from "Lardner's cabinet cyclopedia." cf. Pref.

Narrative of discovery and adventure in the polar seas and regions , with illustrations of their climate, geology, and natural history, and an account of the whale-fishery.

Added t.p., illus.

Narrative of discovery and adventure in the polar seas and regions ...

Added t.-p., illustrated: Discovery and adventure ...

Narrative of discovery and adventure in the Polar seas and regions with illustrations of their climate, geology, and natural history : and an account of the whale-fishery /

Mode of access: Internet.

(Tables S1,2) Stable isotopes in muscle tissue of polar bears (Ursus maritimus) from various regions of the Arctic

The relative contribution of regional contamination versus dietary differences to geographic variation in polar bear (Ursus maritimus) contaminant levels is unknown. Dietary variation between Alaska, Canada, East Greenland, and Svalbard subpopulations was assessed by muscle nitrogen and carbon stable isotope (d15N, d13C) and adipose fatty acid (FA) signatures relative to their main prey (ringed seals). Western and southern Hudson Bay signatures were characterized by depleted d15N and d13C, lower proportions of C20 and C22 monounsaturated FAs and higher proportions of C18 and longer chain polyunsaturated FAs. East Greenland and Svalbard signatures were reversed relative to Hudson Bay. Alaskan and Canadian Arctic signatures were intermediate. Between-subpopulation dietary differences predominated over interannual, seasonal, sex, or age variation. Among various brominated and chlorinated contaminants, diet signatures significantly explained variation in adipose levels of polybrominated diphenyl ether (PBDE) flame retardants (14-15%) and legacy PCBs (18-21%). However, dietary influence was contaminant class-specific, since only low or nonsignificant proportions of variation in organochlorine pesticide (e.g., chlordane) levels were explained by diet. Hudson Bay diet signatures were associated with lower PCB and PBDE levels, whereas East Greenland and Svalbard signatures were associated with higher levels. Understanding diet/food web factors is important to accurately interpret contaminant trends, particularly in a changing Arctic.