Do more banking offices mean more banking services?

An argument that recent growth in the number of banking offices (head offices plus their branches) does not necessarily mean that banking services have increased.Banks and banking - Customer services

Sinergitas Lembaga Pengelola Lingkungan Hidup pada Pemerintah Kabupaten Banyuwangi dalam Mengendalikan Pencemaran Lingkungan Akibat Limbah Pengolahan Ikan di Muncar

Industri pengolahan ikan di Muncar telah meningkatkan kesejahteraan masyarakat setempat dan memberikan peluang kerja yang cukup luas. Industri pengolahan ikan selain meningkatkan kesejahteraan masyarakat setempat dan pendapatan daerah, tetapi juga telah menimbulkan dampak negatif terhadap lingkungan sekitarnya. Rendahnya pemahaman akan IPAL (instalasi pengolahan air limbah) dan sistem manajemen limbah menyebabkan sulitnya untuk mengelola limbah yang ada, sehingga hampir semua limbah yang dihasilkan langsung dibuang ke saluran umum. Pembuangan limbah secara langsung dan tanpa pengelohan ini menyebabkan tingginya tingkat pencemaran lingkungan di sekitar lokasi industri

Ecosystem effects of CO2 concentration: evidence from past climates

Atmospheric CO2 concentration has varied from minima of 170-200 ppm in glacials to maxima of 280-300 ppm in the recent interglacials. Photosynthesis by C-3 plants is highly sensitive to CO2 concentration variations in this range. Physiological consequences of the CO2 changes should therefore be discernible in palaeodata. Several lines of evidence support this expectation. Reduced terrestrial carbon storage during glacials, indicated by the shift in stable isotope composition of dissolved inorganic carbon in the ocean, cannot be explained by climate or sea-level changes. It is however consistent with predictions of current process-based models that propagate known physiological CO2 effects into net primary production at the ecosystem scale. Restricted forest cover during glacial periods, indicated by pollen assemblages dominated by non-arboreal taxa, cannot be reproduced accurately by palaeoclimate models unless CO2 effects on C-3-C-4 plant competition are also modelled. It follows that methods to reconstruct climate from palaeodata should account for CO2 concentration changes. When they do so, they yield results more consistent with palaeoclimate models. In conclusion, the palaeorecord of the Late Quaternary, interpreted with the help of climate and ecosystem models, provides evidence that CO2 effects at the ecosystem scale are neither trivial nor transient

Projected changes in Australian fire regimes during the 21st century and consequences for ecosystems

Climate projections show Australia becoming significantly warmer during the 21st century, while precipitation decreases over much of the continent. Such changes are generally considered to increase wildfire risk. Nevertheless, using a process-based model of vegetation dynamics and vegetation–fire interactions, we show that while burnt area increases in southern and central Australia, it decreases in northern Australia. Overall the projected increase in fire by the end of the 21st century is small (0.7–1.3% of land area equivalent to 12–24% of current burnt area, depending on the climate scenario). The direct effects of increasing CO2 on vegetation productivity and water-use efficiency influence simulated fire regimes: CO2 effects tend to increase burnt area in arid regions, but increase vegetation density and reduce burnt area in forested regions. Increases in fire promotes a shift to more fire-adapted trees in wooded areas and their encroachment into grasslands, with an overall increase in forested area of 3.9–11.9% of land area by the end of the century. The decrease in fire in northern Australia leads to an increase in tree cover (ca 20%) and an expansion of tropical forest. Thus, although the overall change in burnt area is small it has noticeable consequences for vegetation patterns across the continent

SISAL: bringing added value to Speleothem research

Isotopic records from speleothems are an important source of information about past climates and, given the increase in the number of isotope-enabled climate models, are likely to become an important tool for climate model evaluation. SISAL (Speleothem Isotopes Synthesis and Analysis) have created a global database of isotopic records from speleothems in order to facilitate regional analyses and data-model comparison. The papers in this Special Issue showcase the use of the database for regional analyses. In this paper, we discuss some of the important issues underpinning the use of speleothems and how the existence of this database assists palaeoclimate research. We also highlight some of the lessons learned in the creation of the SISAL database and outline potential research going forward

Underlying causes of Eurasian mid-continental aridity in simulations of mid-Holocene climate

The CMIP5/PMIP3 mid-Holocene simulations show drier conditions in the Eurasian mid-continent and a significant increase in summer temperature; in contrast, paleoenvironmental data (including lake level, vegetation and isotope records, and aeolian deposits) and quantitative climate reconstructions show that the mid-continental extratropics were wetter than today and summers were cooler (Harrison et al., 2015). Eurasian mid-continental aridity and warming has been a persistent feature of model simulations, already present in atmosphere-only simulations (Yu & Harrison, 1996) and appearing more strongly in coupled ocean-atmosphere simulations (e.g. Braconnot et al., 2007b; Wohlfahrt et al., 2008; Harrison et al., 2015) and further exacerbated by vegetation feedback (Wohlfarht et al., 2004). The consistency among multiple lines of paleoenvironmental evidence makes it unlikely that the mismatch reflects misinterpretation of the data. Regional temperature biases in the CMIP5 20th century simulations have been linked to biases in surface energy and water balances, with over- or under-prediction of moisture fluxes and evapotranspiration leading to cold and warm temperature biases respectively (Mueller & Seneviratne, 2014). This suggests that discrepancies in the simulation of mid-Holocene climates might have a similar cause. In this paper, we investigate the processes involved in mid-continental climate changes in the CMIP5/PMIP3 simulations in order to identify the underlying cause of the mismatch with observations

SISTEM INFORMASI MANAJEMEN AKADEMIK PADA SMA NEGERI 1 PALEMBANG

Tujuan dilaksanakannya skripsi ini adalah untuk membuat Sistem Informasi Manajemen Akademik pada SMA Negeri 1 Palembang. Penulis membangun sebuah Sistem menggunakan Visual Studio 2008 dan Microsoft SQL Server 2008. Metodologi yang digunakan adalah metodologi iterasi, yang terdiri dari tahap perencanaan sistem, tahap analisis, tahap perancangan, dan tahap implementasi. Identifikasi masalah ditunjukkan dengan pembuatan kerangka PIECES, kebutuhan user digambarkan dengan use case diagram dan glosarium use case. Metode perancangan proses dengan menggambarkan Diagram Konteks dan Diagram Aliran Data Sistem, pemodelan data dengan menggunakan ERD, rancangan antarmuka program sebagai penghubung antara user dan database. Sistem ini diharapkan dapat mempermudah dalam pengambilan keputusan

Full and Partial Knowledge Sharing on Intra-Organizational Broadcast Media

Knowledge sharing, along with its potential predictors, has been a popular research topic. This research extends prior research by examining potential predictors of knowledge sharing together within a more comprehensive model with two additional contexts: the type of recipient of the knowledge is the recipients of intraorganizational broadcast media, and the type of knowledge sharing behavior (full knowledge sharing and partial knowledge sharing). The results of this study suggest that what predicts knowledge sharing behaviors depends on the type of knowledge sharing behavior when considering why people share their knowledge through intra-organizational broadcast media. We explore theoretical implications and future research avenues

The Reading Palaeofire Database: an expanded global resource to document changes in fire regimes from sedimentary charcoal records

This research has been supported by the Leverhulme Trust (grant no. RC-2018-023), the European Research Council (grant no. 694481), the German Research Foundation (grant no. FE-1096/6-1), the Swiss Government Excellence Postdoctoral Scholarships (grant no. FIRECO 2016.0310), the National Science Centre of Poland (grant no. 2015/17/B/ST10/01656), the SCIEX Scholarship Fund (grant no. PSPB-013/2010), and the Estonian Research Council (grant no. MOBJD313).Sedimentary charcoal records are widely used to reconstruct regional changes in fire regimes through time in the geological past. Existing global compilations are not geographically comprehensive and do not provide consistent metadata for all sites. Furthermore, the age models provided for these records are not harmonised and many are based on older calibrations of the radiocarbon ages. These issues limit the use of existing compilations for research into past fire regimes. Here, we present an expanded database of charcoal records, accompanied by new age models based on recalibration of radiocarbon ages using IntCal20 and Bayesian age-modelling software. We document the structure and contents of the database, the construction of the age models, and the quality control measures applied. We also record the expansion of geographical coverage relative to previous charcoal compilations and the expansion of metadata that can be used to inform analyses. This first version of the Reading Palaeofire Database contains 1676 records (entities) from 1480 sites worldwide. The database (RPDv1b – Harrison et al., 2021) is available at https://doi.org/10.17864/1947.000345.Leverhulme Trust RC-2018-023European Research Council (ERC) European Commission 694481German Research Foundation (DFG) FE-1096/6-1Swiss Government Excellence Postdoctoral Scholarships FIRECO 2016.0310SCIEX Scholarship Fund PSPB-013/2010Estonian Research Council MOBJD31