bluuebunny/crossref_metadata_2025_split huggingface dataset:
Revisiting the alignment typology of ditransitive constructions in Chinese dialects
Authors: Zhang Min 
Published: February 2015

With data from over a thousand regional varieties of Chinese, the paper presents a comprehensive survey of ditransitive constructions in Chinese dialects and their alignment types, focusing in particular on delving in system-internal and external factors correlating with the observed typological distinctions. It starts with questioning the validity of one of Hashimoto’s (1976) well-known parameters for North-South typological classification of Chinese – i.e., the double object construction (DOC) takes the form of V-OR-OT in Northern Chinese and V-OT-OR in Southern Chinese, the latter also known as the ‘Inverted DOC’ (IDOC), – based on the fact that two distinct groups of Southern Chinese, i.e., Min and Southwestern Mandarin spoken in Southwestern China, tally unexpectedly with Northern Chinese and only allow the form of V-OR-OT. It is subsequently found that the distinction is strongly correlated with the typology of the generalpurpose verb of giving (the verb ‘to give’). All dialects with DOC possess an underived ditransitive verb ‘to give’, whereas those with IDOC in general lack such as verb, using instead the combination of a monotransitive handling verb and an allative preposition, i.e., the dative construction in the form of ‘take OT to OR’, to express the ‘give’-type ditransitive event. This finding naturally leads to the following conclusions: (1) it is the loss of the verb ‘to give’ that triggers the loss of DOC in the latter group of dialects, which consequently renders the dative construction as the only ‘give’-type ditransitive construction in such dialects; (2) the IDOC is in nature an indirective construction (dative construction) with merely the dative marker left out, and the driving force of the omission is nothing but a high usage frequency of the indirective construction.
It is further observed that the English-like dative alternation between the DOC and the dative construction existing in Chinese for thousands of years since Archaic Chinese is only preserved in a small fraction of its modern varieties. The majority of Chinese dialects have undergone a typological shift from the mixed type to either the DOC-type (predominantly Northern Chinese) or the indirectivetype (predominantly Southern Chinese), motivated by the systerm-external factor (Altaization of Northern Chinese in the former case) and the systerm-internal factor (loss of the verb ‘to give’ in the latter case) respectively
On the Etyma of maŋ2 nau5 “Steamed Rice” in Xia Pu Dialect and A Related Issue
Authors: Wu Rui-wen 
Published: February 2015

According to this author’s fieldwork in Pei Pi Village（北壁鄉），Xia Pu County（霞浦縣），a very interesting finding is that unlike most Chinese dialects, the cognate 飯‘puŋ6’ is not used to mean “steamed rice” but to mean “breakfast”. The word to indicate “steamed rice” is a rare disyllable “maŋ2 nau5” among Eastern Min dialects. This phenomenon is worthy to be looked into by increasing review of dialect materials and expanding the comparative scope.
Through correspondence with ancient Chinese phonological system, this paper aims to demonstrate that the etyma of the disyllable “maŋ2 nau5” are 暝 and 晝 respectively. The compound “maŋ2 nau5” consisted of two elements: the former (which indicates “dinner”) is “maŋ2”, and the latter “nau5” denoted “lunch.” It is obvious that the lexical replacement occurred in Xia Pu dialect. From the lexical shift point of view, the innovation of the replacement is induced by the semantic confusion between “puŋ6”[飯] and “tsa3”[早]. The process of the replacement could be reconstructed as follows:
Further, the etymon of “steamed rice” in several north Eastern Min dialects seems not to be explained reasonably until now, for instance, Fu An “maŋ5”, Zhe Reng “maŋ5”, Shou Ning “maŋ5”, Zhou Ning “maŋ5”. The disyllable “maŋ2 nau5” in Xia Pu may bring the puzzle into light. In view of historical comparison, I have every reason to speculate that “maŋ5” in north Eastern Min dialects could be traced back to the primitive form “maŋ2 nau5”. The phonological strategy is syllable contraction.
The Design Concept and the Phonological System of Huangji Jingshi: Shengyin Changhe Tu: On the Influence of Image-Number Yijing Studies on the Creation of the Korean Alphabet
Authors: Wang Sung-Mu 
Published: February 2015

Among the extant rhyme tables of the Song Dynasty, Shao Yong’s (1011–1077) Huangji Jingshi: Shengyin Changhe Tu is the most unique. It is different from other phonological tables, such as Yunjing and Qiyin Lue, that were designed for the interpretation of fanqie formulae in terms of arrangement and phonological terminology. However, most contemporary scholars have failed to notice the unique design in Shengyin Changhe Tu and merely follow Karlgren’s paradigm, which contends that a phonological table objectively reflects certain dialectal phonological features through the prism of historical phonology.
Instead, the present paper approaches the question of how the rhyme table is structured from the perspective of the history of phonological philosophy rather than historical phonology. By so doing, the role of philologists is reconsidered as that of a rhyme designer constructing an ideal sound system, rather than that of a dialectologist investigating a real sound system. The following questions are then discussed: What is the purpose for compiling such a work as Shengyin Changhe Tu and what are its design motivations? Can other scholars’ reconstructions of the sound system and sound values of Shengyin Changhe Tu be considered reasonable? In addition to Shengyin Changhe Tu, did the Image-Number Yijing School have any impact on the design of the later phonological tables? In this way the author wishes to develop a new humanistic approach toward understanding of the rhyme tables in order to correct the blind spots and flaws resulting from an overly extreme tendency toward scientism.
Re-examining the Devoicing of Middle Chinese Voiced Initials in Hakka: When and Where?
Authors: Kwok Bit-Chee 
Published: February 2015

The voiced stops and affricates of Middle Chinese have basically shifted to their voiceless aspirated counterparts (henceforth, “devoicing”) regardless of tone categories in the following dialects:
1. the Hakka dialects;2. the Gan dialects;3. various Mandarin dialects spoken along the Shanxi-Shaanxi-Henan border;4. a small group of Mandarin dialects in southeastern Jiangsu; and5. a northwestern dialect spoken in the Late Tang period.It has been claimed that the above-mentioned dialects are closely related, based on the fact that they have undergone the same development of the Middle Chinese voiced stops and affricates. In this paper, we argue that the devoicing of Hakka took place in southern China, probably in modern-day southern Jiangxi, some time between the early 10th century and the late 17th century. The devoicing pattern shared by Hakka and other Chinese dialects should therefore be treated as parallel development rather than as evidence for closer genetic affinity among all these dialects.
Column-Integrated Moist Static Energy Budget Analysis on Various Time Scales during TOGA COARE
Authors: Inoue Kuniaki , Back Larissa 
Published: February 2015

Abstract
Moist static energy (MSE) budgets on different time scales are analyzed in the TOGA COARE data using Lanczos filters to separate variability with different frequencies. Four different time scales (~2-day, ~5-day, ~10-day, and MJO time scales) are chosen based on the power spectrum of the precipitation and previous TOGA COARE studies. The lag regression-slope technique is utilized to depict characteristic patterns of the variability associated with the MSE budgets on the different time scales.
This analysis illustrates that the MSE budgets behave in significantly different ways on the different time scales. On shorter time scales, the vertical advection acts as a primary driver of the recharge–discharge mechanism of column MSE. As the time scale gets longer, in contrast, the relative contributions of the other budget terms become greater, and consequently, on the MJO time scale all the budget terms have nearly the same amplitude. Specifically, these results indicate that horizontal advection plays an important role in the eastward propagation of the MJO during TOGA COARE. On the MJO time scale, the export of MSE by the vertical advection is in phase with the precipitation. On shorter time scales, the vertical velocity profile transitions from bottom heavy to top heavy, while on longer time scales, the shape becomes more constant and similar to a first-baroclinic-mode structure. This leads to a more-constant gross moist stability on longer time scales, which the authors estimate.
Estimating the Anthropogenic Sea Surface Temperature Response Using Pattern Scaling
Authors: Bichet Adeline , Kushner Paul J. , Mudryk Lawrence , Terray Laurent , Fyfe John C. 
Published: February 2015

Abstract
This study seeks to derive the sea surface temperature (SST) response to anthropogenic forcing from observations over the last century, using simple methods inspired from pattern scaling. As in pattern scaling, the spatial response is assumed to scale with global-mean and annual-mean surface temperature. The long-term aim of this work is to generate anthropogenically forced SST and sea ice patterns for the recent past and near-term future, and use them to force atmosphere–land climate models for attribution and prediction purposes. The present work compares estimation methodologies and, within a Monte Carlo framework based on large initial condition ensembles of climate model simulations, examines the robustness of the patterns obtained.
The different methods explored here yield a similar SST spatial response, mostly reflecting the observed SST linear trend map. The different methods nevertheless provide distinctive temporal evolution of the global-mean and annual-mean SST response, which in turn affects the temporal evolution of the global-mean and annual-mean air surface temperature simulated in corresponding prescribed SST simulations. The estimated SST spatial response consists mostly of a warming of the midlatitude coasts near the western boundary currents, the tropical Indian Ocean, and the Arctic Ocean. This pattern generally agrees with previously published observational and modeling studies. Based on Monte Carlo analysis of the large ensembles, it is found that between 36% and 56% of its spatial variance results from anthropogenic forcing.
Overall, the work herein provides constraints on the uncertainty associated with the spatial variability of an anthropogenically forced component of climate change derived from observations, which can potentially be used for climate attribution and prediction.
Optimization of a Radiative Transfer Forward Operator for Simulating SMOS Brightness Temperatures over the Upper Mississippi Basin
Authors: Lievens H. , Al Bitar A. , Verhoest N. E. C. , Cabot F. , De Lannoy G. J. M. , Drusch M. , Dumedah G. , Hendricks Franssen H.-J. , Kerr Y. , Tomer S. K. , Martens B. , Merlin O. , Pan M. , van den Berg M. J. , Vereecken H. , Walker J. P. , Wood E. F. , Pauwels V. R. N. 
Published: February 2015

AbstractThe Soil Moisture Ocean Salinity (SMOS) satellite mission routinely provides global multiangular observations of brightness temperature TB at both horizontal and vertical polarization with a 3-day repeat period. The assimilation of such data into a land surface model (LSM) may improve the skill of operational flood forecasts through an improved estimation of soil moisture SM. To accommodate for the direct assimilation of the SMOS TB data, the LSM needs to be coupled with a radiative transfer model (RTM), serving as a forward operator for the simulation of multiangular and multipolarization top of the atmosphere TBs. This study investigates the use of the Variable Infiltration Capacity model coupled with the Community Microwave Emission Modelling Platform for simulating SMOS TB observations over the upper Mississippi basin, United States. For a period of 2 years (2010–11), a comparison between SMOS TBs and simulations with literature-based RTM parameters reveals a basin-averaged bias of 30 K. Therefore, time series of SMOS TB observations are used to investigate ways for mitigating these large biases. Specifically, the study demonstrates the impact of the LSM soil moisture climatology in the magnitude of TB biases. After cumulative distribution function matching the SM climatology of the LSM to SMOS retrievals, the average bias decreases from 30 K to less than 5 K. Further improvements can be made through calibration of RTM parameters related to the modeling of surface roughness and vegetation. Consequently, it can be concluded that SM rescaling and RTM optimization are efficient means for mitigating biases and form a necessary preparatory step for data assimilation.
Observational Perspectives from U.S. Climate Reference Network (USCRN) and Cooperative Observer Program (COOP) Network: Temperature and Precipitation Comparison
Authors: Leeper Ronald D. , Rennie Jared , Palecki Michael A. 
Published: February 2015

AbstractThe U.S. Cooperative Observer Program (COOP) network was formed in the early 1890s to provide daily observations of temperature and precipitation. However, manual observations from naturally aspirated temperature sensors and unshielded precipitation gauges often led to uncertainties in atmospheric measurements. Advancements in observational technology (ventilated temperature sensors, well-shielded precipitation gauges) and measurement techniques (automation and redundant sensors), which improve observation quality, were adopted by NOAA’s National Climatic Data Center (NCDC) into the establishment of the U.S. Climate Reference Network (USCRN). USCRN was designed to provide high-quality and continuous observations to monitor long-term temperature and precipitation trends, and to provide an independent reference to compare to other networks. The purpose of this study is to evaluate how diverse technological and operational choices between the USCRN and COOP programs impact temperature and precipitation observations. Naturally aspirated COOP sensors generally had warmer (+0.48°C) daily maximum and cooler (−0.36°C) minimum temperatures than USCRN, with considerable variability among stations. For precipitation, COOP reported slightly more precipitation overall (1.5%) with network differences varying seasonally. COOP gauges were sensitive to wind biases (no shielding), which are enhanced over winter when COOP observed (10.7%) less precipitation than USCRN. Conversely, wetting factor and gauge evaporation, which dominate in summer, were sources of bias for USCRN, leading to wetter COOP observations over warmer months. Inconsistencies in COOP observations (e.g., multiday observations, time shifts, recording errors) complicated network comparisons and led to unique bias profiles that evolved over time with changes in instrumentation and primary observer.
Impact of Loss of U.S. Microwave and Radio Occultation Observations in Operational Numerical Weather Prediction in Support of the U.S. Data Gap Mitigation Activities
Authors: Cucurull Lidia , Anthes Richard A. 
Published: February 2015

Abstract
As the U.S. polar-orbiting satellites NOAA-15, -18, and -19 and NASA’s Aqua satellite reach the ends of their lives, there may be a loss in redundancy between their microwave (MW) soundings, and the Advanced Technology Microwave Sounder (ATMS) on the Suomi–National Polar-Orbiting Partnership (NPP) satellite. With the expected delay in the launch of the next generation of U.S. polar-orbiting satellites, there may be a loss in at least some of the U.S. MW data. There may also be a significant decrease in the number of radio occultation (RO) observations. The mainstay of the global RO system, the COSMIC constellation of six satellites is already past the end of its nominal lifetime. A replacement of RO soundings in the tropics is planned with the launch of COSMIC-2 satellites in 2016. However, the polar constellation of COSMIC-2 will not be launched until 2018 or 2019, and complete funding for this constellation is not assured. Using the NCEP operational forecast system, forecasts for March–April 2013 are carried out in which various combinations of the U.S. MW and all RO soundings are removed. The main results are that the forecasts are only slightly degraded in the Northern Hemisphere, even with all of these observations removed. The decrease in accuracy is considerably greater in the Southern Hemisphere, where the greatest forecast degradation occurs when the RO observations are removed. Overall, these results indicate that the possible gap in RO observations is potentially more significant than the possible gap in the U.S. MW data.
A Review of Planetary Boundary Layer Parameterization Schemes and Their Sensitivity in Simulating Southeastern U.S. Cold Season Severe Weather Environments
Authors: Cohen Ariel E. , Cavallo Steven M. , Coniglio Michael C. , Brooks Harold E. 
Published: February 2015

AbstractThe representation of turbulent mixing within the lower troposphere is needed to accurately portray the vertical thermodynamic and kinematic profiles of the atmosphere in mesoscale model forecasts. For mesoscale models, turbulence is mostly a subgrid-scale process, but its presence in the planetary boundary layer (PBL) can directly modulate a simulation’s depiction of mass fields relevant for forecast problems. The primary goal of this work is to review the various parameterization schemes that the Weather Research and Forecasting Model employs in its depiction of turbulent mixing (PBL schemes) in general, and is followed by an application to a severe weather environment. Each scheme represents mixing on a local and/or nonlocal basis. Local schemes only consider immediately adjacent vertical levels in the model, whereas nonlocal schemes can consider a deeper layer covering multiple levels in representing the effects of vertical mixing through the PBL. As an application, a pair of cold season severe weather events that occurred in the southeastern United States are examined. Such cases highlight the ambiguities of classically defined PBL schemes in a cold season severe weather environment, though characteristics of the PBL schemes are apparent in this case. Low-level lapse rates and storm-relative helicity are typically steeper and slightly smaller for nonlocal than local schemes, respectively. Nonlocal mixing is necessary to more accurately forecast the lower-tropospheric lapse rates within the warm sector of these events. While all schemes yield overestimations of mixed-layer convective available potential energy (MLCAPE), nonlocal schemes more strongly overestimate MLCAPE than do local schemes.
An experimental study of tremolite dissolution rates as a function of pH and temperature: Implications for tremolite toxicity and its use in carbon storage
Authors: Diedrich Tamara , Schott Jacques , Oelkers Eric H. 
Published: February 2015

Steady-state tremolite dissolution rates, at far-from-equilibrium conditions, were measured as a function of aqueous silica and magnesium activity, pH from 1.9 to 6.7, and temperature from 25 to 150ºC. Calcium is released from tremolite faster than either Mg or Si throughout most of the experiments even after these latter elements attained steady-state release rates. The preferential removal of Ca releases fine Mg-Si rich needle-like fibres from the tremolite, probably promoting its toxicity. In contrast, Mg was released in stoichiometric or near to stoichiometric proportion to Si once steady-state was attained. Measured steady-state tremolite dissolution rates based on Si release can be described using
where r+ signifies the BET surface area-normalized forward tremolite steady-state dissolution rate, AA refers to a pre-exponential factor = 6610–3 mol cm–2 s–1, EA designates an activation energy equal to 80 kJ mol–1, R represents the gas constant, T denotes absolute temperature, and ai refers to the activity of the subscripted aqueous species. This rate expression is consistent with tremolite dissolution rates at acidic pH being controlled by the detachment of partially liberated silica tetrahedra formed from the exchange of Mg2+ for two protons near the mineral surface after the near-surface Ca has been removed. Nevertheless, Mg release rates from tremolite are ~3 orders of magnitude slower than those from forsterite and enstatite suggesting that tremolite carbonation will be far less efficient than the carbonation of these other Mg-silicate minerals.
Second-generation PLINK: rising to the challenge of larger and richer datasets
Authors: Chang Christopher C , Chow Carson C , Tellier Laurent CAM , Vattikuti Shashaank , Purcell Shaun M , Lee James J 
Published: February 2015

Abstract

Background
PLINK 1 is a widely used open-source C/C++ toolset for genome-wide association studies (GWAS) and research in population genetics. However, the steady accumulation of data from imputation and whole-genome sequencing studies has exposed a strong need for faster and scalable implementations of key functions, such as logistic regression, linkage disequilibrium estimation, and genomic distance evaluation. In addition, GWAS and population-genetic data now frequently contain genotype likelihoods, phase information, and/or multiallelic variants, none of which can be represented by PLINK 1's primary data format.

Findings
To address these issues, we are developing a second-generation codebase for PLINK. The first major release from this codebase, PLINK 1.9, introduces extensive use of bit-level parallelism, (n)-time/constant-space Hardy-Weinberg equilibrium and Fisher's exact tests, and many other algorithmic improvements. In combination, these changes accelerate most operations by 1-4 orders of magnitude, and allow the program to handle datasets too large to fit in RAM. We have also developed an extension to the data format which adds low-overhead support for genotype likelihoods, phase, multiallelic variants, and reference vs. alternate alleles, which is the basis of our planned second release (PLINK 2.0).

Conclusions
The second-generation versions of PLINK will offer dramatic improvements in performance and compatibility. For the first time, users without access to high-end computing resources can perform several essential analyses of the feature-rich and very large genetic datasets coming into use.