Nature and degree of aqueous alteration in CM and CI carbonaceous chondrites     

Driss Takir  Joshua P. Emery  Harry Y. Mcsween Jr.  Charles A. Hibbitts  Roger N. Clark  Neil Pearson  Alian Wang 《Meteoritics & planetary science》2013,48(9):1618-1637

We investigated the petrologic, geochemical, and spectral parameters that relate to the type and degree of aqueous alteration in nine CM chondrites and one CI (Ivuna) carbonaceous chondrite. Our underlying hypothesis is that the position and shape of the 3 μm band is diagnostic of phyllosilicate mineralogy. We measured reflectance spectra of the chondrites under dry conditions (elevated temperatures) and vacuum (10^?8 to 10^?7 torr) to minimize adsorbed water and mimic the space environment, for subsequent comparison with reflectance spectra of asteroids. We have identified three spectral CM groups in addition to Ivuna. “Group 1,” the least altered group as determined from various alteration indices, is characterized by 3 μm band centers at longer wavelengths, and is consistent with cronstedtite (Fe‐serpentine). “Group 3,” the most altered group, is characterized by 3 μm band centers at shorter wavelengths and is consistent with antigorite (serpentine). “Group 2” is an intermediate group between group 1 and 3. Ivuna exhibits a unique spectrum that is distinct from the CM meteorites and is consistent with lizardite and chrysotile (serpentine). The petrologic and geochemical parameters, which were determined using electron microprobe analyses and microscopic observations, are found to be consistent with the three spectral groups. These results indicate that the distinct parent body aqueous alteration environments experienced by these carbonaceous chondrites can be distinguished using reflectance spectroscopy. High‐quality ground‐based telescopic observations of Main Belt asteroids can be expected to reveal not just whether an asteroid is hydrated, but also details of the alteration state.  相似文献   

Annual floods in New England (USA) and Atlantic Canada: synoptic climatology and generating mechanisms   总被引：1，自引：1，他引：0  

Mathias J. Collins  Johnathan P. Kirk  Joshua Pettit  Arthur T. DeGaetano  M. Sam McCown  Thomas C. Peterson 《自然地理学》2014,35(3):195-219

New England and Atlantic Canada are characterized by mixed flood regimes that reflect different storm types, antecedent land surface conditions, and flood seasonality. Mixed flood regimes are known to complicate flood risk analyses, yet the synoptic climatology and precipitation mechanisms that generate annual floods in this region have not been described in detail. We analyzed a set of long-term annual flood records at climate-sensitive stream gauges across the region and classified the synoptic climatology of each annual flood, quantitatively describing the precipitation mechanisms, and characterize flood seasonality. We find that annual floods here are dominantly generated by Great Lakes-sourced storms and Coastal lows, known locally as ‘nor’easters.’ Great Lakes storms tend to be associated with lower magnitude annual floods (<75th percentile) and Coastal lows are more clearly associated with higher magnitude events (>75th percentile). Tropical cyclones account for few of all annual floods, including extreme events, despite causing some of the region’s largest and most destructive floods. Late winter/early spring is when the greatest number of annual floods occur region wide, and rainfall is the dominant flood-producing mechanism. Rainfall in combination with snowmelt is also important. Both mechanisms are expected to be impacted by projected regional climate change. We find little evidence for associations between flood-producing synoptic storm types or precipitation mechanisms and large-scale atmospheric circulation indices or time periods, despite upward trends in New England annual flood magnitudes. To more completely investigate such associations, partial duration flood series that include more floods than just the largest of each year, and their associated synoptic climatologies and precipitation mechanisms, should be analyzed.  相似文献   

Landscape position and spatial patterns in the distribution of land use within the southern Appalachian Mountains   总被引：1，自引：1，他引：0  

Joshua S. Rice  Ryan E. Emanuel 《自然地理学》2014,35(5):443-457

Understanding the forces that influence the distribution of land use and land-use change (LUC) is an essential step in developing effective strategies for managing these issues. We examined the influence of landscape position on spatial patterns in land-use distribution within the Little Tennessee River Basin (LTRB) of the southern Appalachian Mountains. We show that landscape position, defined with respect to both natural and anthropogenic spatial variables, provides for the identification of statistically significant differences in the distribution of common forms of land use in the study region. Using the same variables, significant differences in the landscape positions subject to land-use change in the LTRB are also examined. These results suggest landscape position exerts a strong influence on the distribution of different forms of land use and the likeliness of given area undergoing LUC. The approach presented here, of considering land use as a function of landscape position that responds to both natural and anthropogenic forces, may prove useful in aiding the development of future strategies to address the consequences of land use in many regions.  相似文献   

“Story-Networks” of Livestock and Climate Change: Actors,Their Artifacts,and the Shaping of Urban Print Media     

Keith Chun Leem Lee  Joshua Peter Newell  Jennifer Wolch  Nicole Schneider  Pascale Joassart-Marcelli 《社会与自然资源》2014,27(9):948-963

Despite widespread media coverage of livestock-related issues and growing scientific evidence linking meat production and climate change, systematic content analysis of this relationship in media coverage has been surprisingly minimal. In this article, we combine actor-network theory with framing theory to develop the basis for “story-networks”—networks of actants and artifacts that shape how a media report or “story” is framed. We coded livestock-related articles from a major U.S. newspaper, the Los Angeles Times, over the 1999–2010 period to understand how various actants and artifacts shaped different story-networks. Just 5% of all livestock articles addressed connections with climate change; these articles focused on technology, lifestyle, or policy. Distinctive story-networks characterized each category, framing the livestock–climate change linkage as an issue to be addressed through either technological innovation, individual lifestyle choices, or policy action. In each story-network type, varying configurations of actants and artifacts were involved, including the cattle themselves.  相似文献   

Symbol Store: sharing map symbols for emergency management     

Anthony C. Robinson  Scott Pezanowski  Sarah Troedson  Raechel Bianchetti  Justine Blanford  Joshua Stevens 《制图学和地理信息科学》2013,40(5):415-426

Maps are a primary means for supporting information sharing and collaboration in emergency management and crisis situations. While a variety of formalized map symbol standards for emergency contexts exist, they have not been widely adopted by mapmakers. Informal symbol conventions are commonly used within emergency management stakeholder groups, but until now there has not been a flexible mechanism for discovering, sharing, and previewing these symbol sets among mapmakers. In this paper, we describe the design and development of the Symbol Store, a visually enabled, web-based interactive tool intended to help mapmakers share point symbols. The Symbol Store allows users to browse symbols by keyword, category tags, and contributors. It also allows for symbols to be previewed on realistic maps prior to download. An initial prototype of the Symbol Store was evaluated by flood mapping experts from the State of California, and the results of this user study led to multiple refinements now implemented in the public version of Symbol Store located at www.symbolstore.org.  相似文献   

Seasonal snow cover decreases young water fractions in high Alpine catchments     

Natalie Ceperley  Giulia Zuecco  Harsh Beria  Luca Carturan  Anthony Michelon  Daniele Penna  Joshua Larsen  Bettina Schaefli 《水文研究》2020,34(25):4794-4813

Estimation of young water fractions (F_yw), defined as the fraction of water in a stream younger than approximately 2–3 months, provides key information for water resource management in catchments where runoff is dominated by snowmelt. Knowing the average dependence of summer flow on winter precipitation is an essential context for comparing regional drought severity and provides the hydrological template for downstream water users and ecosystems. However, F_yw estimation based on seasonal signals of stable isotopes of oxygen and hydrogen has not yet explicitly addressed how to parsimoniously include the seasonal shift of water input from snow. Using experimental data from three high-elevation, Alpine catchments (one dominated by glacier and two by snow), we propose a framework to explicitly include the delays induced by snow storage into estimates of F_yw. Scrutinizing the key methodological choices when estimating F_yw from isotope data, we find that the methods used to construct precipitation input signals from sparse isotope samples can significantly impact F_yw. Given this sensitivity, our revised procedure estimates a distribution of F_yw values that incorporates a wide range of possible methodological choices and their uncertainties; it furthermore compares the commonly used amplitude ratio approach to a direct convolution approach, which circumvents the assumption that the isotopic signals have a sine curve shape, an assumption that is generally violated in snow-dominated environments. Our new estimates confirm that high-elevation Alpine catchments have low F_yw values, spanning from 8 to 11%. Such low values have previously been interpreted as the impact of seasonal snow storage alone, but our comparison of different F_yw estimation methods suggests that these low F_yw values result from a combination of both snow cover effects and longer storage in the subsurface. In contrast, in the highest elevation, glacier dominated catchment, F_yw is 3–4 times greater compared to the other two catchments, due to the lower storage and faster drainage processes. A future challenge, capturing spatio-temporal snowmelt isotope signals during winter baseflow and the snowmelt period, remains to improve constraints on the F_yw estimation technique.  相似文献   

A process-based approach to attribution of historical streamflow decline in a data-scarce and human-dominated watershed     

Gopal Penny  Veena Srinivasan  R. Apoorva  Kirubaharan Jeremiah  Joshua Peschel  Sierra Young  Sally Thompson 《水文研究》2020,34(8):1981-1995

Human activities have resulted in rapid hydrological change around the world, in many cases producing shifts in the dominant hydrological processes, confounding predictions, and complicating effective management and planning. Identifying and characterizing such changes in hydrological processes is therefore a globally relevant problem, one that is particularly challenging in sparsely monitored environments. We develop a novel, process-based approach for attribution of hydrological change in such scenarios and apply the approach to the TG Halli watershed outside Bangalore, India, where streamflow has declined considerably over the last 50 years. The approach consists of (a) employing a range of field instrumentation and experiments to identify contemporary streamflow generation mechanisms, (b) using these observations to constrain our understanding and generate hypotheses pertaining to historical changes, and (c) evaluating these hypotheses with a range of evidence including proxies for historical hydrological processes. The body of evidence in the TG Halli watershed indicates the historical presence and subsequent loss of a shallow groundwater table that previously discharged to the stream, meaning that groundwater depletion is the most likely driver of streamflow decline. These findings present a viable path towards improved predictions of future water resources and sustainable water management within the watershed. Our process-based approach to attribution has the potential to improve understanding of human-driven hydrological change in regions with poor monitoring of hydrological systems.  相似文献   

Biogeochemical responses over 37 years to manipulation of phosphorus concentrations in an Arctic river: The Upper Kuparuk River Experiment     

Frances M. Iannucci  Joshua Beneš  Alexander Medvedeff  William B. Bowden 《水文研究》2021,35(3):e14075

The climate of the Arctic region is changing rapidly, with important implications for permafrost, vegetation communities, and transport of solutes by streams and rivers to the Arctic Ocean. While research on Arctic streams and rivers has accelerated in recent years, long-term records are relatively rare compared to temperate and tropical regions. We began monitoring the upper Kuparuk River in 1983 as part of a long-term, low-level, whole-season phosphorus enrichment of a 4–6 km experimental reach, which was subsequently incorporated into the Arctic Long-Term Ecological Research (Arctic LTER) programme. The phosphorus enrichment phase of the Upper Kuparuk River Experiment (UKRE) ran continuously for 34 seasons, fundamentally altering the community structure and function of the Fertilized reach. The objectives of this paper are to (a) update observations of the environmental conditions in the Kuparuk River region as revealed by long-term, catchment-level monitoring, (b) compare long-term trends in biogeochemical characteristics of phosphorus-enriched and reference reaches of the Kuparuk River, and (c) report results from a new ‘ReFertilization’ experiment. During the UKRE, temperature and discharge did not change significantly, though precipitation increased slightly. However, the UKRE revealed unexpected community state changes attributable to phosphorus enrichment (e.g., appearance of colonizing bryophytes) and long-term legacy effects of these state changes after cessation of the phosphorus enrichment. The UKRE also revealed important biogeochemical trends (e.g., increased nitrate flux and benthic C:N, decreased DOP flux). The decrease in DOP is particularly notable in that this may be a pan-Arctic trend related to permafrost thaw and exposure to new sources of iron that reduce phosphorus mobility to streams and rivers. The trends revealed by the UKRE would have been difficult or impossible to identify without long-term, catchment level research and may have important influences on connections between Arctic headwater catchments and downstream receiving waters, including the Arctic Ocean.  相似文献   

Barrier‐spit geomorphology and inlet dynamics in absence of tides: evolution of the North Pond system,eastern Lake Ontario,New York State          下载免费PDF全文

Christopher R. Mattheus  Joshua K. Fowler  Thomas P. Diggins  Derrick F. Allen 《地球表面变化过程与地形》2016,41(10):1386-1398

Barrier systems have received much attention along microtidal oceanic coastlines, where countless studies discuss their evolution in response to Holocene sea‐level rise, storm influence, and anthropogenic impacts. Lacustrine barrier evolution is not as well investigated and little is known about how lake‐specific hydrodynamic processes shape barrier morphology. This study evaluates the evolution of a highly dynamic barrier section along eastern Lake Ontario in the context of varying water levels and winter‐ice covers. Paleoshoreline reconstructions and volumetric analyses of nearshore sedimentation indicate the central portion of the studied North Pond barrier has been breached many times in different locations throughout the last century. Ground‐penetrating radar (GPR) data corroborate mapped locations of former inlets, bound at the surface by recurved spit and dune ridges. Subsurface structural controls on inlet position are inferred from a spatial correlation with buried incised fluvial channels, formed during a Holocene lake‐level lowstand. While subsurface controls caused two separate historical inlets to remain stationary while open, an episode of rapid inlet migration elsewhere along the barrier was facilitated by the prevailing direction of coastal currents and high lake levels, which favored overwash and rapid longshore sediment mobility across a low‐gradient barrier section. Additionally, the sudden closing of an inlet after many decades of operation coincidental with the opening of another suggestively occurred alongside unusually high lake levels. These correlations suggest the degree of coastal inundation, predominantly a function of fluctuating lake levels and antecedent topography, represent strong controls on overall barrier geomorphology over decadal timescales. Copyright © 2016 John Wiley & Sons, Ltd.  相似文献   

Effects of heated effluent on Midwestern US lakes: implications for future climate change     

Joshua J. Mulhollem  Robert E. Colombo  David H. Wahl 《Aquatic Sciences - Research Across Boundaries》2016,78(4):743-753

  相似文献