Superheavy nuclei in relativistic effective Lagrangian model

Isotopic and isotonic chains of superheavy nuclei are analyzed to search for spherical double shell closures beyond Z=82 and N=126 within the new effective field theory model of Furnstahl, Serot, and Tang for the relativistic nuclear many-body problem. We take into account several indicators to identify the occurrence of possible shell closures, such as two-nucleon separation energies, two-nucleon shell gaps, average pairing gaps, and the shell correction energy. The effective Lagrangian model predicts N=172 and Z=120 and N=258 and Z=120 as spherical doubly magic superheavy nuclei, whereas N=184 and Z=114 show some magic character depending on the parameter set. The magicity of a particular neutron (proton) number in the analyzed mass region is found to depend on the number of protons (neutrons) present in the nucleus.

Large enhanced dielectric permittivity in polyaniline passivated core-shell nano magnetic iron oxide by plasma polymerization

Commercial samples of Magnetite with size ranging from 25–30nm were coated with polyaniline by using radio frequency plasma polymerization to achieve a core shell structure of magnetic nanoparticle (core)–Polyaniline (shell). High resolution transmission electron microscopy images confirm the core shell architecture of polyaniline coated iron oxide. The dielectric properties of the material were studied before and after plasma treatment. The polymer coated magnetite particles exhibited a large dielectric permittivity with respect to uncoated samples. The dielectric behavior was modeled using a Maxwell–Wagner capacitor model. A plausible mechanism for the enhancement of dielectric permittivity is proposed

Influence of the electronic shell structure on the elastic scattering of heavy ions

The interatomic potential of the system I - I at intermediate and small distances is calculated from atomic DFS electron densities within a statistical model. Structures in the potential, due to the electronic shells, are investigated. Calculations of the elastic differential scattering cross section for small angles and several keV impact energies show a detailed peak pattern which can be correlated to individual electronic shell interaction.

Model-based objects recognition in man-made environments

We describe a model-based objects recognition system which is part of an image interpretation system intended to assist autonomous vehicles navigation. The system is intended to operate in man-made environments. Behavior-based navigation of autonomous vehicles involves the recognition of navigable areas and the potential obstacles. The recognition system integrates color, shape and texture information together with the location of the vanishing point. The recognition process starts from some prior scene knowledge, that is, a generic model of the expected scene and the potential objects. The recognition system constitutes an approach where different low-level vision techniques extract a multitude of image descriptors which are then analyzed using a rule-based reasoning system to interpret the image content. This system has been implemented using CEES, the C++ embedded expert system shell developed in the Systems Engineering and Automatic Control Laboratory (University of Girona) as a specific rule-based problem solving tool. It has been especially conceived for supporting cooperative expert systems, and uses the object oriented programming paradigm

Cap a un model per interpretar i facilitar l'aprendre: estratègies i recursos per a la reflexió-acció en i des de la pràctica

1.- L'enquadrament d'aquest treball de recerca s'ha fet en i des de la praxis. EI que interessa és descobrir i proposar instruments pedagògics d'ajuda, assequibles i contextualitzats, especialment en el terreny de la comunicació i la interacció Educador-Educand. La metodologia que s'ha fet servir és de caire qualitatiu, etnogràfic, en un enfocament basat en la investigació-acció. La visió de la persona és volgudament holística; els sentiments, els significats, I' orientació personal, I' autodirecció. esdevenen elements centrals. La hipòtesi de treball, en la qual es fonamenta la recerca, podria formular-se així: 'En la pràctica, els Educadors, d'una forma més o menys reflexiva, perceben i interpreten el procés d'aprendre dels Educands; hi intervenen, el mediatitzen; n'avaluen la direcció i l'encert". A partir d'aquest supòsit, l'investigador veu convenient donar resposta a tres qüestions centrals: A) Com comprenem i interpretem els Educadors el procés d'aprendre dels Educands?; B) Quin tipus d'intervenció resultarà adient per promoure i/o facilitar l'aprendre?; C) Amb quins instruments i estratègies comptem per ajudar pedagògicament? 2.- Per llegir l'aprendre, l'investigador fa ús d'un model mental, indispensable per ordenar les dades de l'experiència. Convé, per tant, explicitar-lo, fer-ne ciència, coneixement compartit. En aquesta direcció de treball se li plantegen dos tipus d'interrogants: A) Quins són els elements comuns a qualsevol experiència d'aprenentatge?; Quina mena d'activitat o experiència personal desenvolupen tots els Educands; i B) Com es manifesta aquesta experiència? Amb quins indicadors? Quina mena de "text" llegeix l'Educador per orientar la seva intervenció d'ajuda? 3.- L'aprenentatge. en aquest treball, és considerat per l'investigador com la resultant de tres processos personals: el posicionament, l'estratègia i l'avaluació. Quan l'Educador vol compartir amb l'Educand el seu procés idiosincràtic d'aprendre, procura reconstruir amb ell aquestes tres accions bàsiques: A) Com es posiciona: què tem o desitja, què creu, què espera, quines expectatives viu, com es motiva? B) Quines són les seves pautes d'actuació: com treballa, com memoritza, com recupera la informació que té a la memòria, què fa davant d'un problema... ? C) Què busca; què és important per a ella; què pretén... ? 4.- Davant la complexitat dels missatges emesos per l'Educand l'investigador opta per llegir tres tipus de "textos": els productes i els resultats; les conductes; i els missatges parlats. Entre tots tres, pensa, podrà trobar elements i indicadors adequats per fonamentar, sempre hipotèticament, la seva actuació pedagògica. 5.- Procura sobretot detectar i fer existir els èxits, aquells productes i/o resultats que l'Educand troba valuosos, per tal d'ajudar-lo a prendre consciència dels seu repertori personal d'estratègies i capacitats. En aquest àmbit es proposen tres actituds o enfocaments del treball d'ajuda: A) El primer fa referència a la presa de consciència de l'estratègia personal, que s'amaga darrera el producte valorat. B) El segon apunta cap al respecte per l'estratègia que cadascú executa i, per tant, li és familiar. L'Educand la necessita. Es la seva. Es troba en la seva experiència, encara que no necessàriament existeixi en la seva construcció conscient. C) El tercer ,el duu a valorar l'estratègia d'acord amb les finalitats de l'Educand. La seva adequació es legitima pel que es proposa. Partim del supòsit que tota conducta es troba dirigida per un propòsit a vegades difícil de copsar i no sempre recomanable per a l'Educand. 6.- La conducta percebuda de l'Educand és entesa com un missatge, un conjunt d'indicadors de la seva activitat contextualitzada, interna i externa; missatge que, en relació amb altres, com els productes i les verbalitzacions, manifesta fragments dels seus significats, projectes, estratègies, valors. Es fa un èmfasi especial en les conductes "internes", els gestos mentals, l'acció interior, tramesa per mitja de microcomportaments sovint no conscient, i certificada per mitjà de la verbalització del viscut. 7.- Parlar amb l'Educand suposa dues menes d'accions: escoltar i emetre. Escoltem per comprendre; emetem per perfilar la comprensió i també per ajudar. En l'emissió, el missatge pedagògic té dues funcions: a) rellançar i orientar el pensament i l'autoexploració de l'Educand; i b) influir per tal que desenvolupi amb èxit el seu projecte d'aprendre. Interessa d'una manera especial ajudar a integrar en la consciència de l'Educand aquests elements de la seva experiència que poden facilitar-li l'adquisició del coneixement. I entenem que, en aquesta empresa, la paraula i la interacció verbal poden tenir-hi un joc important. Per aquesta raó s'ha considerat necessari oferir un model d'anàlisi de la interacció i els missatges verbals. 8.- "Les persones aprenen sempre, amb recursos, processos i sistemes de valoració idiosincràtics, per fa qual cosa la seva orientació en el context esdevé un referent central en el disseny de l'ajuda pedagògica i en la seva avaluació". Aquesta és la hipòtesi de sortida per dissenyar la intervenció pedagògica. Tothom aprèn, inevitablement; la qüestió és quina cosa està aprenent i de quina manera els seus resultats d'ara són mediatitzats per l'experiència passada i, alhora, condicionen el seu aprendre futur. L'aprenent es posiciona, anticipa el procés d' aprendre, valora la seva. capacitat per desenvolupar-lo amb èxit, es motiva en una determinada direcció, d'acord amb la seva experiència, els seus aprenentatges anteriors. Executa estratègies, mostra un tipus d'intel·ligència, una forma personal de processar la informació. Pretén quelcom. És un sistema obert en relació amb el medi: hi ha uns valors que dirigeixen la seva presa de decisions. Utilitza uns criteris propis, una gamma personal d'opcions conscients. Avalua el que fa, el resultat que obté i la seva capacitat personal. 9.- L'ajuda pedagògica que I' autor proposa s'encamina sobretot a facilitar en l'Educand la descoberta dels seus propis recursos. Es tracta de portar-lo cap a la consideració atenta de la seva pròpia experiència, per amplificar-la i fer-la existir com a recurs conscient . Ha dibuixat i experimentat tres conjunts d'intervenció cadascun enfocat vers un àmbit de l'experiència d'aprendre, el qual col·loca com a prioritari, sense oblidar qualsevol dels altres que pugui ser rellevant, per comprendre o ajudar. A) Intervenció sobre el posicionament. En aquest àmbit enfoca l'estil de motivació que executa l'Educand, mira de corregir-lo, si cal, a partir de l'anàlisi i la comprensió de les seves formes de motivar-se quan ell viu l'èxit. Treballa proposant objectius paradoxals de fracàs gairebé impossible, buscant l'assoliment de petits èxits, potser aparentment insignificants, però estratègics; prescriu l'automatisme, per modificar-lo si l'Educand ho desitja; comprova el procés d'anticipació de I' experiència que l'aprenent es construeix per orientar-se; l'ajuda a contextualitzar anticipació i a fer ús dels seus Ilenguatges interns més eficaços i còmodes;... B) Intervenció sobre les estratègies i processos. En un segon enfocament, no necessàriament posterior al descrit, considera les estratègies de I'Educand, també a partir dels seus encerts i èxits. Mira de portar-lo cap a fa descripció i presa de consciència de les seves maneres de fer mes còmodes i segures, les que lliguen amb les seves preferències cerebrals. Quan viu dificultats, el convida a explorar les excepcions, els moments en els quals les seves realitzacions són satisfactòries. Pretén sobretot modificar les seves creences limitants, posant-lo en conflicte amb els fets de l'experiència. A vegades, caldrà facilitar l'adquisició d'estratègies i procediments nous que l'Educand considera plausibles. Es tracta específicament de fer existir opcions noves d'actuació per tal d'assolir allò que vol i/o necessita. C) Intervenció sobre el sistema de valors de l'Educand. L'Educand viu uns valors, els quals expliquen el seu món intern les conductes que realitza i els resultats que obté. Aquest àmbit és col·locat, en el model, al centre del procés d'aprendre. Hom actua amb propòsits determinats, no necessariament conscients. L'obertura de la persona a l'experiència d'aprendre es dirigeix segons criteris i valors irrenunciables. 10.- L 'Educador procura compartir els objectius de l'Educand i els seus projectes per assolir-los; vol tanmateix que se'n faci coneixedor i director responsable. Per a això li convé preguntar-se per quina mena d'experiència està desenvolupant i quin sentit ecològic te per a ell. L'Educador, el seu model del món, la seva persona, està compromès en el procés d'ajuda. No és només un tècnic que aplica recursos objectius. El seu model de comunicació, el seu pensament, les seves expectatives i anticipacions, tenen un pes considerable en el tipus d'intervenció pedagògica que durà a terme i, d'escreix, en el tipus d' aprenentatge que facilita. En la intervenció, l'Educador parteix d'una avaluació intencionadament positiva, centrada en els recursos i les solucions, en la metacognició i l'autoregulació dels processos, a partir de premisses que pressuposen l'èxit personal.

An Assessment of the Recent Past and Future Climate Change, Glacier Retreat, and Runoff in the Caucasus Region Using Dynamical and Statistical Downscaling and HBV-ETH Hydrological Model

The paper discusses the observed and projected warming in the Caucasus region and its implications for glacier melt and runoff. A strong positive trend in summer air temperatures of 0.05 degrees C a(-1) is observed in the high-altitude areas providing for a strong glacier melt and continuous decline in glacier mass balance. A warming of 4-7 degrees C and 3-5 degrees C is projected for the summer months in 2071-2100 under the A2 and B2 emission scenarios respectively, suggesting that enhanced glacier melt can be expected. The expected changes in winter precipitation will not compensate for the summer melt and glacier retreat is likely to continue. However, a projected small increase in both winter and summer precipitation combined with the enhanced glacier melt will result in increased summer runoff in the currently glaciated region of the Caucasus (independent of whether the region is glaciated at the end of the twenty-first century) by more than 50% compared with the baseline period.

Glacier shrinkage and climatic change in the Russian Altai from the mid-20th century: An assessment using remote sensing and PRECIS regional climate model

This paper examines changes in the surface area of glaciers in the North and South Chuya Ridges, Altai Mountains in 1952-2004 and their links with regional climatic variations. The glacier surface areas for 2004 were derived from the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) imagery. Data from the World Glacier Inventory (WGI)dating to 1952 and aerial photographs from 1952 were used to estimate the changes. 256 glaciers with a combined area of 253±5.1 km2 have been identified in the region in 2004. Estimation of changes in extent of 126 glaciers with the individual areas not less than 0.5 km2 in 1952 revealed a 19.7±5.8% reduction. The observed glacier retreat is primarily driven by an increase in summer temperatures since the 1980s when air temperatures were increasing at a rate of 0.10 - 0.13oC a-1 at the glacier tongue elevation. The regional climate projections for A2 and B2 CO2 emission scenarios developed using PRECIS regional climate model indicate that summer temperatures will increase in the Altai in 2071-2100 by 6-7oC and 3-5oC respectively in comparison with 1961-1990 while annual precipitation will increase by 15% and 5%. The length of the ablation season will extend from June-August to the late April – early October. The projected increases in precipitation will not compensate for the projected warming and glaciers will continue to retreat in the 21st century under both B2 and A2 scenarios.

Understanding projections of sea level rise in a Hadley Centre coupled climate model

Sea level changes resulting from CO2-induced climate changes in ocean density and circulation have been investigated in a series of idealised experiments with the Hadley Centre HadCM3 AOGCM. Changes in the mass of the ocean were not included. In the global mean, salinity changes have a negligible effect compared with the thermal expansion of the ocean. Regionally, sea level changes are projected to deviate greatly from the global mean (standard deviation is 40% of the mean). Changes in surface fluxes of heat, freshwater and wind stress are all found to produce significant and distinct regional sea level changes, wind stress changes being the most important and the cause of several pronounced local features, while heat and freshwater flux changes affect large parts of the North Atlantic and Southern Ocean. Regional change is related mainly to density changes, with a relatively small contribution in mid and high latitudes from change in the barotropic circulation. Regional density change has an important contribution from redistribution of ocean heat content. In general, unlike in the global mean, the regional pattern of sea level change due to density change appears to be influenced almost as much by salinity changes as by temperature changes, often in opposition. Such compensation is particularly marked in the North Atlantic, where it is consistent with recent observed changes. We suggest that density compensation is not a property of climate change specifically, but a general behavior of the ocean.

Multi-model assessment of stratospheric ozone return dates and ozone recovery in CCMVal-2 models

Projections of stratospheric ozone from a suite of chemistry-climate models (CCMs) have been analyzed. In addition to a reference simulation where anthropogenic halogenated ozone depleting substances (ODSs) and greenhouse gases (GHGs) vary with time, sensitivity simulations with either ODS or GHG concentrations fixed at 1960 levels were performed to disaggregate the drivers of projected ozone changes. These simulations were also used to assess the two distinct milestones of ozone returning to historical values (ozone return dates) and ozone no longer being influenced by ODSs (full ozone recovery). The date of ozone returning to historical values does not indicate complete recovery from ODSs in most cases, because GHG-induced changes accelerate or decelerate ozone changes in many regions. In the upper stratosphere where CO2-induced stratospheric cooling increases ozone, full ozone recovery is projected to not likely have occurred by 2100 even though ozone returns to its 1980 or even 1960 levels well before (~2025 and 2040, respectively). In contrast, in the tropical lower stratosphere ozone decreases continuously from 1960 to 2100 due to projected increases in tropical upwelling, while by around 2040 it is already very likely that full recovery from the effects of ODSs has occurred, although ODS concentrations are still elevated by this date. In the midlatitude lower stratosphere the evolution differs from that in the tropics, and rather than a steady decrease in ozone, first a decrease in ozone is simulated from 1960 to 2000, which is then followed by a steady increase through the 21st century. Ozone in the midlatitude lower stratosphere returns to 1980 levels by ~2045 in the Northern Hemisphere (NH) and by ~2055 in the Southern Hemisphere (SH), and full ozone recovery is likely reached by 2100 in both hemispheres. Overall, in all regions except the tropical lower stratosphere, full ozone recovery from ODSs occurs significantly later than the return of total column ozone to its 1980 level. The latest return of total column ozone is projected to occur over Antarctica (~2045–2060) whereas it is not likely that full ozone recovery is reached by the end of the 21st century in this region. Arctic total column ozone is projected to return to 1980 levels well before polar stratospheric halogen loading does so (~2025–2030 for total column ozone, cf. 2050–2070 for Cly+60×Bry) and it is likely that full recovery of total column ozone from the effects of ODSs has occurred by ~2035. In contrast to the Antarctic, by 2100 Arctic total column ozone is projected to be above 1960 levels, but not in the fixed GHG simulation, indicating that climate change plays a significant role.

Geodetic mass balance of Azarova glacier, Kodar Mountains, eastern Siberia, and its links to observed and projected climatic change

The Kodar Mountains in eastern Siberia accommodate 30 small, cold-based glaciers with a combined surface area of about 19 km2. Very little is known about these glaciers, with the first survey conducted in the late 1950s. In this paper, we use terrestrial photogrammetry to calculate changes in surface area, elevation, volume and geodetic mass balance of the Azarova Glacier between 1979 and 2007 and relate these to meteorological data from nearby Chara weather station (1938-2007). The glacier surface area declined by 20±6.9% and surface lowered on average by 20±1.8 m (mean thinning: 0.71 m a-1) resulting in a strongly negative cumulative and average mass balance of -18±1.6 m w.e. and -640±60 mm w.e.a-1 respectively. The July-August air temperature increased at a rate of 0.036oC a-1 between 1979 and 2007 and the 1980-2007 period was, on average, around 1oC warmer than 1938-1979. The regional climate projections for A2 and B2 CO2 emission scenarios developed using PRECIS regional climate model indicate that summer temperatures will increase in 2071–2100 by 2.6-4.7°C and 4.9-6.2°C respectively in comparison with 1961–1990. The annual total of solid precipitation will increase by 20% under B2 scenario but decline by 3% under A2 scenario. The length of the ablation season will extend from July–August to June-September. The Azarova Glacier exhibits high sensitivity to climatic warming due to its low elevation, exposure to comparatively high summer temperatures, and the absence of a compensating impact of cold season precipitation. Further summer warming and decline of solid precipitation projected under the A2 scenario will force Azarova to retreat further while impacts of an increase in solid precipitation projected under the B2 scenario require further investigation.

Model inter-comparison between statistical and dynamic model assessments of the long-term stability of blanket peat in Great Britain (1940-2099)

We compared output from 3 dynamic process-based models (DMs: ECOSSE, MILLENNIA and the Durham Carbon Model) and 9 bioclimatic envelope models (BCEMs; including BBOG ensemble and PEATSTASH) ranging from simple threshold to semi-process-based models. Model simulations were run at 4 British peatland sites using historical climate data and climate projections under a medium (A1B) emissions scenario from the 11-RCM (regional climate model) ensemble underpinning UKCP09. The models showed that blanket peatlands are vulnerable to projected climate change; however, predictions varied between models as well as between sites. All BCEMs predicted a shift from presence to absence of a climate associated with blanket peat, where the sites with the lowest total annual precipitation were closest to the presence/absence threshold. DMs showed a more variable response. ECOSSE predicted a decline in net C sink and shift to net C source by the end of this century. The Durham Carbon Model predicted a smaller decline in the net C sink strength, but no shift to net C source. MILLENNIA predicted a slight overall increase in the net C sink. In contrast to the BCEM projections, the DMs predicted that the sites with coolest temperatures and greatest total annual precipitation showed the largest change in carbon sinks. In this model inter-comparison, the greatest variation in model output in response to climate change projections was not between the BCEMs and DMs but between the DMs themselves, because of different approaches to modelling soil organic matter pools and decomposition amongst other processes. The difference in the sign of the response has major implications for future climate feedbacks, climate policy and peatland management. Enhanced data collection, in particular monitoring peatland response to current change, would significantly improve model development and projections of future change.

Bioclimatic envelope model of climate change impacts on blanket peatland distribution in Great Britain

Blanket peatlands are rain-fed mires that cover the landscape almost regardless of topography. The geographical extent of this type of peatland is highly sensitive to climate. We applied a global process-based bioclimatic envelope model, PeatStash, to predict the distribution of British blanket peatlands. The model captures the present areal extent (Kappa = 0.77) and is highly sensitive to both temperature and precipitation changes. When the model is run using the UKCIP02 climate projections for the time periods 2011–2040, 2041–2070 and 2071–2100, the geographical distribution of blanket peatlands gradually retreats towards the north and the west. In the UKCIP02 high emissions scenario for 2071–2100, the blanket peatland bioclimatic space is ~84% smaller than contemporary conditions (1961–1990); only parts of the west of Scotland remain inside this space. Increasing summer temperature is the main driver of the projected changes in areal extent. Simulations using 7 climate model outputs resulted in generally similar patterns of declining aereal extent of the bioclimatic space, although differing in degree. The results presented in this study should be viewed as a first step towards understanding the trends likely to affect the blanket peatland distribution in Great Britain. The eventual fate of existing blanket peatlands left outside their bioclimatic space remains uncertain.

A comparative analysis of projected impacts of climate change on river runoff from global and catchment-scale hydrological models

We present a comparative analysis of projected impacts of climate change on river runoff from two types of distributed hydrological model, a global hydrological model (GHM) and catchment-scale hydrological models (CHM). Analyses are conducted for six catchments that are global in coverage and feature strong contrasts in spatial scale as well as climatic and development conditions. These include the Liard (Canada), Mekong (SE Asia), Okavango (SW Africa), Rio Grande (Brazil), Xiangu (China) and Harper's Brook (UK). A single GHM (Mac-PDM.09) is applied to all catchments whilst different CHMs are applied for each catchment. The CHMs typically simulate water resources impacts based on a more explicit representation of catchment water resources than that available from the GHM, and the CHMs include river routing. Simulations of average annual runoff, mean monthly runoff and high (Q5) and low (Q95) monthly runoff under baseline (1961-1990) and climate change scenarios are presented. We compare the simulated runoff response of each hydrological model to (1) prescribed increases in global mean temperature from the HadCM3 climate model and (2)a prescribed increase in global-mean temperature of 2oC for seven GCMs to explore response to climate model and structural uncertainty. We find that differences in projected changes of mean annual runoff between the two types of hydrological model can be substantial for a given GCM, and they are generally larger for indicators of high and low flow. However, they are relatively small in comparison to the range of projections across the seven GCMs. Hence, for the six catchments and seven GCMs we considered, climate model structural uncertainty is greater than the uncertainty associated with the type of hydrological model applied. Moreover, shifts in the seasonal cycle of runoff with climate change are presented similarly by both hydrological models, although for some catchments the monthly timing of high and low flows differs.This implies that for studies that seek to quantify and assess the role of climate model uncertainty on catchment-scale runoff, it may be equally as feasible to apply a GHM as it is to apply a CHM, especially when climate modelling uncertainty across the range of available GCMs is as large as it currently is. Whilst the GHM is able to represent the broad climate change signal that is represented by the CHMs, we find, however, that for some catchments there are differences between GHMs and CHMs in mean annual runoff due to differences in potential evaporation estimation methods, in the representation of the seasonality of runoff, and in the magnitude of changes in extreme monthly runoff, all of which have implications for future water management issues.

Dependence of Indian monsoon rainfall on moisture fluxes across the Arabian Sea and the impact of coupled model sea surface temperature biases

The Arabian Sea is an important moisture source for Indian monsoon rainfall. The skill of climate models in simulating the monsoon and its variability varies widely, while Arabian Sea cold sea surface temperature (SST) biases are common in coupled models and may therefore influence the monsoon and its sensitivity to climate change. We examine the relationship between monsoon rainfall, moisture fluxes and Arabian Sea SST in observations and climate model simulations. Observational analysis shows strong monsoons depend on moisture fluxes across the Arabian Sea, however detecting consistent signals with contemporaneous summer SST anomalies is complicated in the observed system by air/sea coupling and large-scale induced variability such as the El Niño-Southern Oscillation feeding back onto the monsoon through development of the Somali Jet. Comparison of HadGEM3 coupled and atmosphere-only configurations suggests coupled model cold SST biases significantly reduce monsoon rainfall. Idealised atmosphere-only experiments show that the weakened monsoon can be mainly attributed to systematic Arabian Sea cold SST biases during summer and their impact on the monsoon-moisture relationship. The impact of large cold SST biases on atmospheric moisture content over the Arabian Sea, and also the subsequent reduced latent heat release over India, dominates over any enhancement in the land-sea temperature gradient and results in changes to the mean state. We hypothesize that a cold base state will result in underestimation of the impact of larger projected Arabian Sea SST changes in future climate, suggesting that Arabian Sea biases should be a clear target for model development.

A review on Northern Hemisphere sea-ice, storminess and the North Atlantic Oscillation: observations and projected changes

The Arctic has undergone substantial changes over the last few decades in various cryospheric and derivative systems and processes. Of these, the Arctic sea ice regime has seen some of the most rapid change and is one of the most visible markers of Arctic change outside the scientific community. This has drawn considerable attention not only from the natural sciences, but increasingly, from the political and commercial sectors as they begin to grapple with the problems and opportunities that are being presented. The possible impacts of past and projected changes in Arctic sea ice, especially as it relates to climatic response, are of particular interest and have been the subject of increasing research activity. A review of the current knowledge of the role of sea ice in the climate system is therefore timely. We present a review that examines both the current state of understanding, as regards the impacts of sea-ice loss observed to date, and climate model projections, to highlight hypothesised future changes and impacts on storm tracks and the North Atlantic Oscillation. Within the broad climate-system perspective, the topics of storminess and large-scale variability will be specifically considered. We then consider larger-scale impacts on the climatic system by reviewing studies that have focused on the interaction between sea-ice extent and the North Atlantic Oscillation. Finally, an overview of the representation of these topics in the literature in the context of IPCC climate projections is presented. While most agree on the direction of Arctic sea-ice change, the rates amongst the various projections vary greatly. Similarly, the response of storm tracks and climate variability are uncertain, exacerbated possibly by the influence of other factors. A variety of scientific papers on the relationship between sea-ice changes and atmospheric variability have brought to light important aspects of this complex topic. Examples are an overall reduction in the number of Arctic winter storms, a northward shift of mid-latitude winter storms in the Pacific and a delayed negative NAO-like response in autumn/winter to a reduced Arctic sea-ice cover (at least in some months). This review paper discusses this research and the disagreements, bringing about a fresh perspective on this issue.