Dynamic characteristics of Atmospheric boundary Layer during different phases of Monsoon

Atmospheric Boundary layer (ABL) is the layer just above the earth surface and is influenced by the surface forcing within a short period of an hour or less. In this thesis, characteristics of the boundary layer over ocean, coastal and inland areas of the atmosphere, especially over the monsoon regime are thoroughly studied. The study of the coastal zone is important due to its high vulnerability mainly due to sea breeze circulation and associated changes in the atmospheric boundary layer. The major scientific problems addressed in this thesis are diurnal and seasonal variation of coastal meteorological properties, the characteristic difference in the ABL during active and weak monsoons, features of ABL over marine environment and the variation of the boundary layer structure over an inland station. The thesis describes the various features in the ABL associated with the active and weak monsoons and, the surface boundary layer properties associated with the active and weak epochs. The study provides knowledge on MABL and can be used as the estimated values of boundary layer parameters over the marine atmosphere and to know the values and variabilities of the ABL parameters such as surface wind, surface friction, drag coefficient, wind stress and wind stress curl.

Thermal transport across incommensurate phases in potassium selenate: photo-pyroelectric and calorimetric measurements

The thermal transport properties—thermal diffusivity, thermal conductivity and specific heat capacity—of potassium selenate crystal have been measured through the successive phase transitions, following the photo-pyroelectric thermal wave technique. The variation of thermal conductivity with temperature through the incommensurate (IC) phase of this crystal is measured. The enhancement in thermal conductivity in the IC phase is explained in terms of heat conduction by phase modes, and the maxima in thermal conductivity during transitions is due to enhancement in the phonon mean free path and the corresponding reduction in phonon scattering. The anisotropy in thermal conductivity and its variation with temperature are reported. The variation of the specific heat with temperature through the high temperature structural transition at 745 K is measured, following the differential scanning calorimetric method. By combining the results of photo-pyroelectric thermal wave methods and differential scanning calorimetry, the variation of the specific heat capacity with temperature through all the four phases of K2SeO4 is reported. The results are discussed in terms of phonon mode softening during transitions and phonon scattering by phase modes in the IC phase.

HRTEM assessment of Wurtzite and Zinc-Blende phases in GaAs nanowires for optoelectronic devices

Màster en Nanociència i Nanotecnologia. Curs 2007-2008. Directors: Francesca Peiró i Martínez and Jordi Arbiol i Cobos

Integer filling facfor phases and isospin in vertical diatomic artificial molecules

Integer filling factor phases of many-electron vertically coupled diatomic artificial quantum dot molecules are investigated for different values of the interdot coupling. The experimental results are analyzed within local-spin density functional theory for which we have determined a simple lateral confining potential law that can be scaled for the different coupling regimes, and Hartree-Fock theory. Maximum density droplets composed of electrons in both bonding and antibonding or just bonding states are revealed, and interesting isospin-flip physics appears for weak interdot coupling when the systematic depopulation of antibonding states leads to changes in isospin.

Characteristics of ABL during active and weak phases of monsoon

Understanding of the Atmospheric Boundary Layer (ABL) is imperative in the arena of the monsoon field. Here, the features of the ABL are studied employing Conserved Variable Analysis (CVA) using equivalent potential temperature and humidity. In addition, virtual potential temperature and wind are used during active and weak phases of monsoon. The analysis is carried out utilising the radiosonde observations during the monsoon months for two stations situated in the west coast of India. All these parameters show considerable variations during active and weak monsoon phases in both the stations. The core speed and core height vary with these epochs. The core speed is found to be more than 38 knots in the active monsoon phase around 1.2 km over Trivandrum and around 2 km over Mangalore. But during weak monsoon phase the core wind speed is decreased and core height is elevated over both stations. The wind direction shows an additional along shore component during weak monsoon period. The Convective Boundary Layer (CBL) height shows increase during weak monsoon phase over both stations due to less cloudiness and subsequent insolation. The CBL height during the southwest monsoon is more over Mangalore and is attributed by the orographic lifting in the windward side of the Western Ghats while the influence of the Ghats is less over Trivandrum.

Computer-mediated communication and time pressure induce higher cardiovascular responses in the preparatory and execution phases of cooperative tasks

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Estructura i ultraestructura testicular del mascle reproductor porcí (Sus domesticus)

El present treball analitza al microscopi òptic i al microscopi electrònic de transmissió el testicle de Sus domesticus (raça Landrace - varietat anglesa) a partir de mascles reproductors porcins adults i sans. L'objectiu principal de tots els centres d'Inseminació Artificial Porcina i de les Explotacions de Selecció i Multiplicació Porcina és garantir una excel·lent qualitat espermàtica al llarg de la vida reproductiva útil d'un mascle reproductor porcí. Així doncs, un millor coneixement dels patrons estructural i ultraestructural normals del testicle permetrà diagnosticar amb facilitat quina ha estat l'estructura o funció testicular afectada quan s'observa una disminució de la qualitat del semen. Les anàlisis seminals i hormonals són certament crucials en la valoració d'aquests mascles, però, no són totalment informatives de les alteracions testiculars, ja que és necessari conèixer l'organització microscòpica. Diversos estudis sobre testicle han demostrat que els marcadors més sensibles per a l'avaluació de la funció testicular són els següents: (1) la grandària testicular, (2) el gruix i l'organització de la càpsula testicular, (3) el percentatge de túbuls seminífers i de teixit intersticial en el parènquima testicular, (4) el diàmetre dels túbuls seminífers, (5) l'alçada i la composició de cèl·lules germinals de l'epiteli seminífer, (6) el gruix i l'organització de la làmina pròpia i, (7) la morfologia i la grandària de les cèl·lules de Leydig. El primer objectiu concret del present estudi ha estat, per tant, caracteritzar tots aquests paràmetres testiculars en mascles porcins sans i adults. L'organització estructural del testicle i les mesures quantitatives utilitzades com a marcadors no mostren diferències significatives ni entres els mascles porcins (P > 0,01), ni entre el testicle dret i l'esquerre (P > 0,01). Els testicles, de 330,80  16,99 g de pes, estan envoltats per una càpsula, de 2.375,13  246,68 m de gruix, la qual es divideix en tres capes: la túnica vaginalis constitueix l'1,82  0,78 % de la càpsula i està composta per una capa mesotelial externa i una capa interna de teixit conjuntiu dens; la túnica albuginea representa el 37,31  3,27 % i és de teixit conjuntiu dens i, la túnica vasculosa constitueix el 64,24 4,40 % i és de teixit conjuntiu lax. En el parènquima testicular els túbuls seminífers i el teixit intersticial representen el 72,44  2,12 % i el 27,46  2,12 %, respectivament. Els túbuls seminífers, de 226,23  18,08 m de diàmetre, es troben fortament recargolats i empaquetats, i estan compostos per la làmina pròpia i l'epiteli seminífer. La làmina pròpia, de 4-4,5 m de gruix, està formada per la làmina basal i dues capes de cèl·lules peritubulars. L'epiteli seminífer, amb una alçada mitjana de 66,11  10,62 m, és columnar i estratificat amb cèl·lules de Sertoli i diferents generacions d'espermatogònies, espermatòcits i espermàtides. El teixit intersticial és un teixit conjuntiu lax amb abundants cèl·lules de Leydig polièdriques fortament empaquetades (ca. 15 x 12 m). El segon objectiu concret d'aquest estudi ha estat estudiar des del punt de vista morfològic i morfomètric (alçada, longitud, freqüència relativa d'aparició i durada) els estadis del cicle de l'epiteli seminífer en els mascles porcins de la raça Landrace (varietat anglesa), classificats d'acord amb el mètode de la morfologia tubular. Els estadis premeiòtics ( I, II i III) ocupen el 31,9 % del cicle espermatogènic i es caracteritzen, principalment, per la presència de cèl·lules en les fase inicials de la meiosi I. Les primeres etapes de la meiosi I no afecten els paràmetres morfomètrics de l'epiteli seminífer ja que els valors obtinguts per l'alçada de l'epiteli seminífer, la freqüència relativa, la longitud i la durada d'aquests estadis són molt variables. Els estadis meiòtics (IV i V) representen el 16,4 % del cicle espermatogènic i estan constituïts, principlament, per cèl·lules en un estat avançat de la meiosi I i /o cèl·lules en meiosi II. Les últimes fases de la meiosi I i també de la meiosi II tenen lloc ràpidament, la qual cosa resulta en una baixa freqüència relativa d'aparició i, per tant, en una baixa durada dels estadis meiòtics. Els estadis postmeiòtics (VI, VII i VIII) ocupen el 50,6 % del cicle espermatogènic. L'esdeveniment més important que té lloc en aquests estadis és la fase de maduració de l'espermiogènesi. En la fase de maduració, les espermàtides experimenten diverses modificacions morfològiques i estructurals que donen lloc, finalment, als espermatozoides. La complexitat d'aquests processos fa que els estadis postmeiòtics presentin valors més grans de freqüència relativa, longitud i durada. El tercer objectiu concret d'aquest treball ha estat descriure a nivell ultraestructural el procés d'espermiogènesi, i relacionar les transformacions que experimenten les espermàtides en fase d'elongació amb els canvis ultraestructurals que tenen lloc en les diferents cèl·lules que constitueixen el testicle (cèl·lules germinals, de Sertoli i de Leydig, principalment). L'espermiogènesi del mascle porcí de la raça Landrace (varietat anglesa) s'ha dividit en 9 passos que vénen definits per 9 tipus diferents d'espermàtides. Al llarg de l'espermiogènesi no s'observen diferències ultraestructurals significatives (P > 0,01) ni entre els mascles porcins ni entre el testicle esquerre i dret en les cèl·lules que constitueixen el testicle.

Multiple phases of North African humidity recorded in lacustrine sediments from the Fazzan Basin, Libyan Sahara

The Fazzan Basin of south-west Libya is at present arid with less than 20 mm of rainfall per annum. However, regionally extensive limestones, lacustrine sands and coquina (fossiliferous carbonate rock) deposits show that the Fazzan Basin previously contained a large palaeolake, indicating that the climate in the past was more humid. Optically stimulated luminescence (OSL) dating techniques have been applied to key lacustrine deposits within the basin in an attempt to provide an internally consistent chronology for this humidity record. Results indicate that palaeolake sediments within the Fazzan Basin record a very long history of palacohydrological change, ranging from present day and conditions to humidity capable of sustaining a lake with an approximate area of 76,250 km(2). The existence of humid periods in mid oxygen isotope stage 5 and the early Holocene is confirmed. An older lacustrine event, tentatively correlated to oxygen isotope stage 11, is also recognized. In addition, evidence is presented for at least two humid phases beyond the age range over which the conventional OSL dating technique is applicable. This study demonstrates that OSL dating of palaeolake sediments within the Fazzan Basin offers the potential to provide a detailed record of North African humidity spanning several glacial-interglacial cycles. (c) 2006 Elsevier Ltd. All rights reserved.

Subglacial bedform evidence for a major palaeo-ice stream and its retreat phases in Amundsen Gulf, Canadian Arctic Archipelago

Ascertaining the location of palaeo-ice streams is crucial in order to produce accurate reconstructions of palaeo-ice sheets and examine interactions with the ocean-climate system. This paper reports evidence for a major ice stream in Amundsen Gulf, Canadian Arctic Archipelago. Mapping from satellite imagery (Landsat ETM+) and digital elevation models, including bathymetric data, is used to reconstruct flow-patterns on southwestern Victoria Island and the adjacent mainland (Nunavut and Northwest Territories). Several flow-sets indicative of ice streaming are found feeding into the marine trough and cross-cutting relationships between these flow-sets (and utilising previously published radiocarbon dates) reveal several phases of ice stream activity centred in Amundsen Gulf and Dolphin and Union Strait. A large erosional footprint on the continental shelf indicates that the ice stream (ca. 1000 km long and ca. 150 km wide) filled Amundsen Gulf, probably at the Last Glacial Maximum. Subsequent to this, the ice stream reorganised as the margin retreated back along the marine trough, eventually splitting into two separate low-gradient lobes in Prince Albert Sound and Dolphin and Union Strait. The location of this major ice stream holds important implications for ice sheet-ocean interactions and specifically, the development of Arctic Ocean ice shelves and the delivery of icebergs into the western Arctic Ocean during the late Pleistocene. Copyright (C) 2006 John Wiley & Sons, Ltd.

Phases of dormancy in yam tubers (Dioscorea rotundata)

center dot Background and Aims The control of dormancy in yam (Disocorea spp.) tubers is poorly understood and attempts to shorten the long dormant period (i.e. cause tubers to sprout or germinate much earlier) have been unsuccessful. The aim of this study was to identify and define the phases of dormancy in Dioscorea rotundata tubers, and to produce a framework within which dormancy can be more effectively studied. center dot Methods Plants of 'TDr 131' derived from tissue culture were grown in a glasshouse simulating temperature and photoperiod at Ibadan (7 degrees N), Nigeria to produce tubers. Tubers were sampled on four occasions: 30 d before shoot senescence (149 days after planting, DAP), at shoot senescence (179 DAP), and twice during storage at a constant 25 degrees C (269 and 326 DAP). The development of the apical shoot bud was described from tissue sections. In addition, the responsiveness of shoot apical bud development to plant growth regulators (gibberellic acid, 2-chloroethanol and thiourea) applied to excised tuber sections was also examined 6 and 12 d after treatment. center dot Key Results and Conclusions Three phases of tuber dormancy are proposed: Phase I, from tuber initiation to the appearance of the tuber germinating meristem; Phase II, from the tuber germinating meristem to initiation of foliar primordium; and Phase III, from foliar primordium to appearance of the shoot bud on the surface of the tuber. Phase I is the longest phase (approx. 220 d in 'TDr 131'), is not affected by PGRs and is proposed to be an endo-dormant phase. Phases II and III are shorter (< 70 d in total), are influenced by PGRs and environmental conditions, and are therefore endo-/eco-dormant phases. To manipulate dormancy to allow off-season planting and more than one generation per year requires that the duration of Phase I is shortened.