Miracle-dz/UniFAR-FTUs huggingface dataset:
Nearshore Bathymetry Derived from Video Imagery

Owing to the economic importance of seasonal fluctuations in beach width and the frequent implementation of local beach and shoreface nourishments, coastal managers and scientists increasingly demand coastal state information at smaller spatiotemporal scales. Advanced, automated video techniques provide the means to collect such high-resolution monitoring data. Successful use of video imagery for coastal monitoring requires the quantification of relevant morphological parameters from remotely sensed information. This thesis presents two complementary methods to quantify intertidal and subtidal beach bathymetry from time-averaged video observations. Application of the new methods to a nourished beach at Egmond (The Netherlands) has confirmed their utility in support of coastal management, revealing unexpected morphodynamic behaviour that would have been hard to measure with traditional survey techniques. Stefan Aarninkhof conducted his PhD. research at the Department of Civil Engineering and Geosciences of Delft University of Technology, in close collaboration with Delft Hydraulics.
Estimation of wind-induced losses from a precipitation gauge network in the Australian Snowy Mountains

AbstractWind-induced losses, or undercatch, can have a substantial impact on precipitation gauge observations, especially in alpine environments that receive a substantial amount of frozen precipitation and may be exposed to high winds. A network of NOAH II all-weather gauges installed in the Snowy Mountains since 2006 provides an opportunity to evaluate the magnitude of undercatch in an Australian alpine environment. Data from two intercomparison sites were used with NOAH II gauges with different configurations of wind fences installed: unfenced, WMO standard double fence intercomparison reference (full DFIR) fences, and an experimental half-sized double fence (half DFIR). It was found that average ambient temperature over 6-h periods was sufficient to classify the precipitation phase as snow, mixed precipitation, or rain in a statistically robust way. Empirical catch ratio relationships (i.e., the quotient of observations from two gauges), based on wind speed, ambient temperature, and measured precipita.
Concrete Performance Using Low-Degradation Aggregates

The durability of Portland cement concrete (PCC) has long been identified as a concern by transportation communities around the United States. In this study, the long-term performance of two batches of concrete incorporating either low-degradation (LD) or normal (NM) aggregates subjected to freezing and thawing conditions was experimentally studied. The freezing and thawing test method (ASTM C666) was followed to condition all the test samples. Dynamic modulus and fracture energy for both groups of concrete samples after different numbers of freeze-thaw cycles were measured through nondestructive modal and cohesive fracture tests, respectively. Due to the higher air content in LD concrete, surface scaling was less severe under frost action. Test results showed that different aggregate degradation has an important effect on the freeze-thaw resistance of the concrete and the rate of decrease in fracture energy with number of freeze-thaw cycles for the LD concrete is higher than for the NM concrete. Compared to the dynamic modulus of elasticity, the fracture energy is a more sensitive parameter for evaluating concrete degradation caused by the frost action. Thus, the degradation of aggregate in concrete can be better evaluated by the cohesive fracture test. Additional research is needed to identify an appropriate threshold for when aggregate degradation properties become a concern. Until that time, it is recommended that WSDOT maintain their current restrictions on using low-degradation aggregates in concrete.
Characteristics of Mineralizing Fluids of the Darreh‐Zerreshk and Ali‐Abad Porphyry Copper Deposits, Central Iran, Determined by Fluid Inclusion Microthermometry

The Darreh‐Zereshk (DZ) and Ali‐Abad (AB) porphyry copper deposits are located in southwest of the Yazd city, central Iran. These deposits occur in granitoid intrusions, ranging in composition from quartz monzodiorite through granodiorite to granite. The ore‐hosting intrusions exhibit intense hydrofracturing that lead to the formation of quartz‐sulfide veinlets. Fluid inclusions in hydrothermal quartz in these deposits are classified as a mono‐phase vapor type (Type I), liquid‐rich two phase (liquid + vapor) type (Type IIA), vapor‐rich two phase (vapor + liquid) type (Type IIB), and multi‐phase (liquid + vapor + halite + sylvite + hematite + chalcopyrite and pyrite) type (Types III). Homogenization temperatures (Th) and salinity data are presented for fluid inclusions from hydrothermal quartz veinlets associated with potassic alteration and other varieties of hypogene mineralization. Ore precipitation occurred between 150° to >600°C from low to very high salinity (1.1–73.9 wt% NaCl equivalent) aqueous fluids. Two stages of hydrothermal activity characterized are recognized; one which shows relatively high Th and lower salinity fluid (Type IIIa; Th(L‐V) > Tm(NaCl)); and one which shows lower Th and higher salinity (Type IIIb; Th(L‐V) < Tm(NaCl)). The high Th(L‐V) and salinities of Type IIIa inclusions are interpreted to represent the initial existence of a dense fluid of magmatic origin. The coexistence of Type IIIb, Type I and Type IIB fluid inclusions suggest that these inclusions resulted either from trapping of boiling fluids and/or represent two immiscible fluids. These processes probably occurred as the result of pressure fluctuations from lithostatic to hydrostatic conditions under a pressure of 200 to 300 bar. Dilution of these early fluids by meteoritic water resulted in lower temperatures and low to moderate salinity (<20 wt% NaCl equiv.) fluids (Type IIA). Fluid inclusion analysis reveals that the hydrothermal fluid, which formed mineralized quartz veinlets in the rocks with potassic alteration, had temperatures of ∼500°C and salinity ∼50 wt% NaCl equiv. Cryogenic SEM‐EDS analyses of frozen and decrepitated ore‐bearing fluids trapped in the inclusions indicate the fluids were dominated with NaCl, and KCl with minor CaCl2.
Quantifying evapotranspiration and its components in a coniferous subalpine forest in Southwest China

Evaporation is one of the most important processes in the soil‐plant‐atmosphere‐continuum water cycle. The objectives of the present study were to (1) test the feasibility of different methods for quantifying evapotranspiration (ET) and its components and (2) investigate and quantify ET and its components in a subalpine watershed from April to October, 2009. Our research site was in the Gongga Mountains, located on the southeastern fringe of the Qinghai‐Tibet Plateau. The components of ET could be observed using the interception, sap‐flow and stable isotope techniques. The summation of these components, referred to as the summed components method, was thought to be the ET. Similar estimates of ET from April to October were obtained using the summed components (736 mm) and Eddy covariance (598 mm) methods. The mean of two ET estimates (667 mm) accounted for 50% of the total water input. ET was composed of 6% soil evaporation, 19% vegetation transpiration and 75% interception evaporation. Copyright © 2011 John Wiley & Sons, Ltd.
Influence of the Monsoon Trough on Westward-Propagating Tropical Waves over the Western North Pacific. Part I: Observations

AbstractThe present study investigates the possible linkage between the monsoon trough and the interannual variability of the activity of westward-propagating tropical waves (WTW) over the western North Pacific (WNP) during July–November for the period 1979–2007. It is shown that the interannual variability of WTW activity is closely related to the location of the monsoon trough. During the years when the enhanced (weakened) monsoon trough extends eastward (retreats westward), the lower-tropospheric WTW activity is above (below) normal within the southeastern quadrant of the WNP. Furthermore, this study evaluates different wave structures and dynamics of two types of WTWs, equatorial Rossby (ER) waves and mixed Rossby–gravity (MRG)–tropical depression (TD)-type waves, in strong monsoon trough (S-MT) and weak monsoon trough (W-MT) years over the WNP. There is a significant change in the three-dimensional structure as those waves propagate westward to the east of the monsoon trough. For the TD–MRG waves, an.
Alteration of hyaloclastites in the HSDP 2 Phase 1 Drill Core: 2. Mass balance of the conversion of sideromelane to palagonite and chabazite

The Hawaii Scientific Drilling Project 2 Phase 1 core permits study of each stage of alteration of basalt glass during burial because stages of the process are separated vertically. Previous work has shown that alteration of hyaloclastite occurs progressively. The latest stage observed in the Phase 1 core involves marginal replacement of sideromelane in shards with palagonite while simultaneously forming chabazite in pores. The basic reaction at this stage is sideromelane + components from pore waters = palagonite + chabazite + components to pore waters. Mass balance calculations show that Fe was virtually immobile in this process, being retained in palagonite. Na, Ca, Ba, P, Al, and Si were lost during palagonitization and not fully consumed in making chabazite. Mg was lost during palagonitization but retained elsewhere in smectite. K, Rb, and Sr were extracted from pore waters and enriched in the sum of the alteration products. The amount of enrichment depended upon the amount of chabazite present, which depended upon the porosity when chabazite formed. Ti, Y, U, Zr, Nb, REE, and Th were enriched in palagonite, compared to sideromelane, but were absent in chabazite. Mass balance of all phases for the entire alteration process (including earlier stages) was not possible because poorly consolidated samples do not yield accurate modal values of phases, trace element analysis of smectite was not possible, and exchange with lavas and intrusions in the succession cannot be evaluated. Calculations indicate that too little of major oxides, except Na2O, was released during palagonitization to account for the amount of smectite observed in hyaloclastites. The results of this study, and several others published in the literature, indicate that under various circumstances palagonitization will consume particular elements from pore fluid or release them to it. Such mobility implies that the hydrology of the particular system and the composition of the dissolved solids in the pore water will control whether palagonitization is a source or sink of elements. The potential exists that palagonitization of basalt glass is an important source or sink of elements for seawater and fluids circulating in the ocean crust.
Opportunity and incentive for becoming bilingual in Colombia: Implications for Programa Nacional de Bilingüismo

The Programa Nacional de Bilingüismo (PNB) seeks to promote English proficiency in Colombian society in order to position Colombia within world communication processes, a global economy, and an increasingly multicultural world. Using documentary and statistical data within a case study approach, we characterize the PNB as a case of acquisition planning and argue that some of the social conditions that bolster bilingualism are not sufficiently developed in the Colombian context. Specifically, we maintain that the number of jobs requiring bilingual workers in Colombia's labor market and the patterns of international mobility of Colombians provide little opportunity and incentive for developing bilingualism to the extent envisioned by the PNB.
Enhancing On-Farm Conservation Of Agro-Biodiversity Through Community Seed Bank: An Experience Of Western Nepal

The community seed bank (CSB) is emerged as an effective rural institution at the community level to strengthen farmers’ access to diversity of crop genetic resources as well as seeds that contribute to local food security for poor farmers and also to ensure the conservation of agro-biodiversity on-farm. This paper presents some evidences from the community of western Nepal to demonstrate that CSB is one of the options to conserve and use agro-biodiversity on farm. Biodiversity Conservation and Development Committees (BCDCs) and farmers have established six CSBs in western terai with the support of Agrobiodiversity component of Western Terai Landscape Complex Project (WTLCP-ABD) in Bardia (1 CSB), Kanchanpur (2 CSBs) and Kailali (3 CSBs) districts. These CSBs are functional with prearranged community developed mechanisms for collection, conservation, replication and distribution of seeds. Communities have collected and conserved 88 (Belwa), 77 (Beldandi), 99 (Gadariya), 78 (Masuriya), 76 (Patharaiya) and 82 (Shankarpur) number of accessions of different crops in CSBs. CSB enhanced farmer’s seed system and strengthened social networks for exchange of seeds to cope with impacts of climatic adversity by providing immediate access to locally adapted germplasm as community based adaptation strategy. CSB is becoming a reliable local adaptation practice that minimizes the potential negative impacts of climate change in addition to accessibility, conservation and use of genetic resources in western terai of Nepal. The Journal of Agriculture and Environment Vol:12, Jun.2011, Page 132-139 DOI: http://dx.doi. org/10.3126/aej.v12i0. 7573
Seasonal variation on physico-chemical parameters and trace metals in groundwater of an industrial area of north Chennai, India

Seasonal variation on physico-chemical parameters and trace metals of groundwater in and around Ambattur industrial area, Chennai were determined. The hydrochemical investigation revealed that the seasonal effect does not change the order of abundance of cations and anions but it does change the concentration of various ions present in the groundwater. Alkali metals (Na + , K + ) and strong acids (Cl - , SO 4 2- ) are dominating over alkaline earth metals (Ca 2+ , Mg 2+ ) and weak acids (HCO 3 - , CO 3 2- ) for both seasons. Statistical analysis indicates the highest positive correlation exists between EC and Cl with correlation co-efficient of 0.97 and 0.96 during pre and post-monsoon respectively. Nitrate concentration in the groundwater ranges from 2 to 258 mg/l during pre-monsoon. in the case of post-monsoon, it ranges from 0 to 230 mg/L. During post-monsoon period, nitrate concentration decreased in many wells that are located mostly inside the industrial area. However, it has increased in the residential area, reflecting that the leaching of nitrate from the open sewerage lines. Groundwater in the study area is generally hard, fresh to brackish and low alkaline nature. The unsuitability of groundwater for drinking was identified in few places due to high total hardness and TDS. Fluoride is within the permissible limit for human consumption as per international standards.
Tectonic analysis of the Honaz Fault (western Anatolia) using geomorphic indices and the regional implications

Honaz Dağı (Honaz Mountain, Denizli) is the highest peak in western Anatolia (2517 m) and represents the southern margin of the Denizli Graben Horst System in the western Anatolia Extensional Province. Honaz Fault is a 2-km-wide, 15-km-long northward arc-shaped dip-slip listric normal fault that bounds the northern margin of Honaz Dağı, and has been formed under an N–S-trending extensional tectonic regime since the early Quaternary. This study uses fieldwork and digital elevation model-based geomorphic analysis to identify the kinematic behaviour of the Honaz Fault. Morphometric indices, such as axial river profiles, drainage basin geometries, triangular facets, mountain‐front lineament patterns and sinuosities, document the impact of active tectonics on the evolution of the Honaz Fault and its surroundings, as do valley floor width-to-height ratios and mountain front facet characteristics. These neotectonic indices suggest a relatively high degree of tectonic activity along the Honaz Fault, and suggest that the Quaternary landscape evolution of Honaz Dağı was governed by structural and climate-related erosional processes. Combined geomorphic indices and field data suggest that the analysed dip-slip normal fault segments of the Honaz Fault are linear and highly active, and could generate earthquakes with magnitudes of 6.7. Morphometric analyses of the fault trace along the mountain front yield minimum slip rates of . 15–. 38 mm/y for the Honaz Fault, which are similar to slip rates calculated for active normal faults in the Aegean region.
Late Cretaceous-Cenozoic history of deciduousness and the terminal Cretaceous event

Deciduousness in mesic, broad-leaved plants occurred in disturbed, middle-latitude environments during the Late Cretaceous. Only in polar environments in the Late Cretaceous was the deciduous element dominant, although of low diversity. The terminal Cretaceous event resulted in wide-spread selection for plants of deciduous habit and diversification of deciduous taxa, thus leaving a lasting imprint on Northern Hemisphere vegetation. Various environmental factors have played important roles in subsequent diversification of mesic, broad-leaved deciduous taxa and in origination and decline of broad-leaved deciduous forests. Low diversity and rarity of mesic deciduous plants in the post-Cretaceous of the Southern Hemisphere indicate that the inferred “impact winter” of the terminal Cretaceous event had little effect on Southern Hemisphere vegetation and climate.
A Simple Automatic Calibration Routine for the HBV Model

A simple, but efficient, method for automatic calibration of the conceptual HBV rainfall-runoff model was developed. A new criterion, which combines the commonly used efficienyy criterion R 2 and the relative volume error was introduced. Optimising this combined criterion resulted in R 2 values nearly as high as those for optimssing only R 2, but with much smaller volume errors. An earlier automatic calibration method for the HBV model relied on the use of differett criteria for different parameters. With the simplification to one single criterion, the optimum search method could be made more efficient. The optimisation is made for one parameter at a time, while the others are kept constant. This one-dimensional optimisation is repeated in a loop for all parameters. A new loop is performed as long as there is a sufficiently large improvement since the last one. After each loop a search is made in the direction which is defined by the differences in parameter values between the two latest loops. The calibration routine was developed for, and tested with, the HBV model, but it should be general enough to be applicable to other modess as well.
Isotopic variations in continental basaltic lavas as indicators of mantle heterogeneity: Examples fr

The nature and significance of Sr and Nd isotopic variations in late Cenozoic basalts from the western U.S. Cordillera region are examined in the light of major and trace element characteristics of two end member suites from the Lunar Crater (LCVF) and the Snake River Plain (SRP) volcanic fields. Like many other late Cenozoic Basin and Range basalts, those from LCVF are mildly alkalic and have isotopic (Sr, Nd) compositions similar to those of many oceanic island basalts (OIB). SRP basaltic lavas are tholeiitic and have lower incompatible trace element contents and systematically higher 87Sr/86Sr and lower 143Nd/144Nd isotopic ratios compared to LCVF lavas. These two suites are unlikely to have any genetic relation to one another but are representative of the range of isotopic variations observed in the region. We specifically address the question of how such isotopic diversity arises. For example, (1) could all of these magmas be generated from isotopically similar source materials and then be variably contaminated by crustal material during ascent, or (2) do their isotopic compositions reflect actual heterogeneities within the underlying mantle? To answer these questions, processes of contamination were evaluated using combined major and trace element and isotopic data, and it is concluded that isotopic distinctions between SRP and LCVF basalts cannot be entirely due to contamination. Indeed, they seem to reflect compositional differences in the respective magma source regions. We interpret the LCVF magmas to represent partial melts of dominantly “asthenospheric” mantle (i.e., similar to OIB sources) which, in the case of the Basin and Range province, has presumably upwelled beneath a region of major lithospheric extension. In contrast, isotopically distinct SRP basalts could be derived from ancient or enriched mantle that most likely resides in the continental lithosphere. Thus lateral and/or vertical heterogeneities inferred to exist in the mantle beneath the western United States can be reconciled with geodynamic models that are consistent with regional tectonic evolution.
The value of high-resolution Met Office regional climate models in the simulation of multi-hourly precipitation extremes

AbstractExtreme value theory is used as a diagnostic for two high-resolution (12-km parameterized convection and 1.5-km explicit convection) Met Office regional climate model (RCM) simulations. On subdaily time scales, the 12-km simulation has weaker June–August (JJA) short-return-period return levels than the 1.5-km RCM, yet the 12-km RCM has overly large high return levels. Comparisons with observations indicate that the 1.5-km RCM is more successful than the 12-km RCM in representing (multi)hourly JJA very extreme events. As accumulation periods increase toward daily time scales, the erroneous 12-km precipitation extremes become more comparable with the observations and the 1.5-km RCM. The 12-km RCM fails to capture the observed low sensitivity of the growth rate to accumulation period changes, which is successfully captured by the 1.5-km RCM. Both simulations have comparable December–February (DJF) extremes, but the DJF extremes are generally weaker than in JJA at daily or shorter time scales. Case st.