Ozone and the polar hood of Mars     

C.A. Barth  M.L. Dick 《Icarus》1974,22(2):205-211

Ozone co-appears with the clouds of the polar hood in the winter hemisphere of Mars, but each is variable from day to day and location.to location. Both the appearance of ozone and the polar hood clouds correlate with the temperature of the atmosphere which varies from day to day and location to location. A cold, clean, dry atmosphere is conducive to the formation of ozone.  相似文献   

Mariner 9 ultraviolet spectrometer experiment: Observations of ozone on Mars     

A.L. Lane  C.A. Barth  C.W. Hord  A.I. Stewart 《Icarus》1973,18(1):102-108

The Mariner 9 Ultraviolet Spectrometer has observed the 2550 Å ozone spectral absorption feature on Mars. This absorption was previously detected in the south polar region by Mariner 7 in 1969. Mariner 9 did not observe ozone at any time in the equatorial region, nor at the south polar cap during its summer season. However, ozone was found in the north polar region beginning at a latitude of 45°N and extending northward. Ozone later appeared in the southern hemisphere southward of 50°S as the Mars autumnal equinox approached. The presence of ozone on Mars seems to be coupled to the water vapor content of its atmosphere.  相似文献   

Summer Field Meeting in Norway: 7–22 August, 1950     

O. Holtedahl  T.F.W. Barth  N-H. Kolderup  A. Kvale  J.F. Kirkaldy 《Proceedings of the Geologists' Association. Geologists' Association》1951,62(3):203-223

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The impact of different cooling strategies on urban air temperatures: the cases of Campinas,Brazil and Mendoza,Argentina     

Noelia?Liliana?AlchaparEmail author  Claudia?Cotrim?Pezzuto  Erica?Norma?Correa  Lucila?Chebel Labaki 《Theoretical and Applied Climatology》2017,130(1-2):35-50

This paper describes different ways of reducing urban air temperature and their results in two cities: Campinas, Brazil—a warm temperate climate with a dry winter and hot summer (Cwa), and Mendoza, Argentina—a desert climate with cold steppe (BWk). A high-resolution microclimate modeling system—ENVI-met 3.1—was used to evaluate the thermal performance of an urban canyon in each city. A total of 18 scenarios were simulated including changes in the surface albedo, vegetation percentage, and the H/W aspect ratio of the urban canyons. These results revealed the same trend in behavior for each of the combinations of strategies evaluated in both cities. Nevertheless, these strategies produce a greater temperature reduction in the warm temperate climate (Cwa). Increasing the vegetation percentage reduces air temperatures and mean radiant temperatures in all scenarios. In addition, there is a greater decrease of urban temperature with the vegetation increase when the H/W aspect ratio is lower. Also, applying low albedo on vertical surfaces and high albedo on horizontal surfaces is successful in reducing air temperatures without raising the mean radiant temperature. The best combination of strategies—60 % of vegetation, low albedos on walls and high albedos on pavements and roofs, and 1.5 H/W—could reduce air temperatures up to 6.4 °C in Campinas and 3.5 °C in Mendoza.  相似文献   

Desertification in the Eastern Province of Saudi Arabia   总被引：1，自引：0，他引：1  

Hans-Jrg Barth 《Journal of Arid Environments》1999,43(4):399

The problem of land degradation in the Eastern Province of Saudi Arabia is not a new phenomenon, but during the last decade it has grown to be a serious threat to the delicate desert ecosystems, and also to the urban and industrial areas, due to an increase in sand movement. The area under investigation is situated on the Gulf coast north of Jubail and is approximately 20 km in width centered along the coastline. The total area is almost 1000 km². Eight vegetation types were classified according to the dominant and co-dominant species. A comparative study of the vegetation in a fenced, non-grazed area and in an open grazed area showed that the impact of grazing and recreational activities have largely reduced the value of the rangelands. The reduction in species diversity and density leads to an increase in wind and sand dynamics. Exposed roots, giant ripples, changes in the extension of inland sabkhas and new active dunes could be observed in many parts of the study area. It could be proved that most inland sabkhas in the area are pure deflational features with considerable dynamic due to the reduction in vegetation cover during the recent years. The monitoring of vegetation density was carried out during helicopter flights with the help of GPS and a video camera. Image processing on a personal computer allowed accurate calculations of vegetation density. Observations on active dune fields in the area showed that the size of the dune fields almost doubled in 15 months. Tests in small enclosures showed that there is a potential for natural recovery even in severely damaged areas. In just one year without grazing and with average precipitation there is a significant difference in vegetation cover. Strict grazing management and camping regulations are required to prevent further degradation and allow the recovery of damaged ecosystems. Community involvement and education is necessary for the development of an understanding of regulations and the need for preservation.  相似文献   

Sounding rocket measurements of the solar soft X-ray irradiance   总被引：1，自引：0，他引：1  

Bailey  S.M.  Woods  T.N.  Canfield  L.R.  Korde  R.  Barth  C.A.  Solomon  S.C.  Rottman  G.J. 《Solar physics》1999,186(1-2):243-257

Measurements of the solar soft X-ray (XUV: 2 nm to 30 nm) irradiance were performed from a sounding rocket payload flown from White Sands Missile Range, New Mexico on 4 October 1993 and again on 3 November 1994. The soft X-ray instrumentation comprised of silicon photodiodes with thin films deposited directly onto their active areas. The deposited material and its thickness in conjunction with the sensitivity of an uncoated diode determine the passband and the sensitivity of these photometric devices. The measurements are interpreted in terms of appropriate SERF 1 (Hinteregger, Fukui, and Gilson, 1981) model solar spectra. It is found that the data are consistent with a solar spectrum that is on average approximately a factor of two times the model solar spectra. It is shown that the measured irradiances are in reasonable agreement with other experiments.  相似文献   

Correction of inertial oscillations by assimilation of HF radar data in a model of the Ligurian Sea   总被引：1，自引：1，他引：0  

Luc Vandenbulcke  Jean-Marie Beckers  Alexander Barth 《Ocean Dynamics》2017,67(1):117-135

This article aims at analyzing if high-frequency radar observations of surface currents allow to improve model forecasts in the Ligurian Sea, where inertial oscillations are a dominant feature. An ensemble of ROMS models covering the Ligurian Sea, and nested in the Mediterranean Forecasting System, is coupled with two WERA high-frequency radars. A sensitivity study allows to determine optimal parameters for the ensemble filter. By assimilating observations in a single point, the obtained correction shows that the forecast error covariance matrix represents the inertial oscillations, as well as large- and meso-scale processes. Furthermore, it is shown that the velocity observations can correct the phase and amplitude of the inertial oscillations. Observations are shown to have a strong effect during approximately half a day, which confirms the importance of using a high temporal observation frequency. In general, data assimilation of HF radar observations leads to a skill score of about 30% for the forecasts of surface velocity.  相似文献   

Pre‐drill Groundwater Geochemistry in the Karoo Basin,South Africa          下载免费PDF全文

Jennifer S. Harkness  Kelley Swana  William K. Eymold  Jodie Miller  Ricky Murray  Siep Talma  Colin J. Whyte  Myles T. Moore  Erica L. Maletic  Avner Vengosh  Thomas H. Darrah 《Ground water》2018,56(2):187-203

Enhanced production of unconventional hydrocarbons in the United States has driven interest in natural gas development globally, but simultaneously raised concerns regarding water quantity and quality impacts associated with hydrocarbon extraction. We conducted a pre‐development assessment of groundwater geochemistry in the critically water‐restricted Karoo Basin, South Africa. Twenty‐two springs and groundwater samples were analyzed for major dissolved ions, trace elements, water stable isotopes, strontium and boron isotopes, hydrocarbons and helium composition. The data revealed three end‐members: a deep, saline groundwater with a sodium‐chloride composition, an old, deep freshwater with a sodium‐bicarbonate‐chloride composition and a shallow, calcium‐bicarbonate freshwater. In a few cases, we identified direct mixing of the deep saline water and shallow groundwater. Stable water isotopes indicate that the shallow groundwater was controlled by evaporation in arid conditions, while the saline waters were diluted by apparently fossil meteoric water originated under wetter climatic conditions. These geochemical and isotopic data, in combination with elevated helium levels, suggest that exogenous fluids are the source of the saline groundwater and originated from remnant seawater prior to dilution by old meteoric water combined with further modification by water‐rock interactions. Samples with elevated methane concentrations (>14 ccSTP/kg) were strongly associated with the sodium‐chloride water located near dolerite intrusions, which likely provide a preferential pathway for vertical migration of deeply sourced hydrocarbon‐rich saline waters to the surface. This pre‐drill evaluation indicates that the natural migration of methane‐ and salt‐rich waters provides a source of geogenic contamination to shallow aquifers prior to shale gas development in the Karoo Basin.  相似文献   

Deep-sea faunal communities associated with a lost intermodal shipping container in the Monterey Bay National Marine Sanctuary,CA     

Josi R. Taylor  Andrew P. DeVogelaere  Erica J. Burton  Oren Frey  Lonny Lundsten  Linda A. Kuhnz  P.J. Whaling  Christopher Lovera  Kurt R. Buck  James P. Barry 《Marine pollution bulletin》2014

Carrying assorted cargo and covered with paints of varying toxicity, lost intermodal containers may take centuries to degrade on the deep seafloor. In June 2004, scientists from Monterey Bay Aquarium Research Institute (MBARI) discovered a recently lost container during a Remotely Operated Vehicle (ROV) dive on a sediment-covered seabed at 1281 m depth in Monterey Bay National Marine Sanctuary (MBNMS). The site was revisited by ROV in March 2011. Analyses of sediment samples and high-definition video indicate that faunal assemblages on the container’s exterior and the seabed within 10 m of the container differed significantly from those up to 500 m. The container surface provides hard substratum for colonization by taxa typically found in rocky habitats. However, some key taxa that dominate rocky areas were absent or rare on the container, perhaps related to its potential toxicity or limited time for colonization and growth. Ecological effects appear to be restricted to the container surface and the benthos within ∼10 m.  相似文献   

Simulation of scree‐slope dynamics: investigating the distribution of debris avalanche events in an idealized two‐dimensional model          下载免费PDF全文

Mike Bithell  Keith S. Richards  Erica G. Bithell 《地球表面变化过程与地形》2014,39(12):1601-1610

We present a two‐dimensional model of the development of scree slopes using the discrete‐element method. We concentrate on the dynamics of the accumulating debris at the cliff foot rather than on the failure modes of the cliff‐face or shape of the underlying rock surface. The evolution of this unconsolidated material is intermittent and systematically changing over time, with an early high disturbance regime, dominated by a characteristic event size (where 65% of particles in the debris are in motion to some extent), replaced at later times by many shallow slides interspersed with infrequent large events that involve motion through almost the full scree depth. These large slides lead to a stratigraphy in which the layers of material are stretched almost horizontal near the base of the slope. The scree surface thus shows a gradient in age with most recent rock‐fall close to the cliff and the oldest rock‐fall debris outcropping at the foot. The final surface slope tends to show little curvature, and the final mean slope is well correlated with the angle of internal friction of the particles, although the change is very small over a wide range of friction angles [final slope (in degrees relative to horizontal) ~ 0.043 × internal friction angle + 17.49, with a correlation coefficient of 0.89, p‐value 0.0001]. Some weak size‐segregation of the debris is found, but this seems to have little to do with individual particles bounding down the slope. The shape of the rock core agrees largely with the analytic forms given by Fisher–Lehmann and Bakker–Le Heux expressions, but the original simple Fisher quadratic can give the best fit. Overall the evolution shows a remarkable insensitivity to the model parameters, suggesting that the controls on dry scree‐slope evolution are primarily geometric in character. Copyright © 2014 John Wiley & Sons, Ltd.  相似文献