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Academic literature on the topic 'Lake Sunrise'

Author: Grafiati
Published: 10 December 2022
Last updated: 28 January 2023

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Journal articles on the topic "Lake Sunrise"

1

Korovessis, Panagiotis. "Sunrise at Pamvotida Lake (Ioannina, Greece)." Spine 40, no. 1 (January 2015): i. http://dx.doi.org/10.1097/01.brs.0000459538.40114.fa.

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2

Li, Zhijun, Qingkai Wang, Mingguang Tang, Peng Lu, Guoyu Li, Matti Leppäranta, Jussi Huotari, Lauri Arvola, and Lijuan Shi. "Diurnal Cycle Model of Lake Ice Surface Albedo: A Case Study of Wuliangsuhai Lake." Remote Sensing 13, no. 16 (August 23, 2021): 3334. http://dx.doi.org/10.3390/rs13163334.

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Ice surface albedo is an important factor in various optical remote sensing technologies used to determine the distribution of snow or melt water on the ice, and to judge the formation or melting of lake ice in winter, especially in cold and arid areas. In this study, field measurements were conducted at Wuliangsuhai Lake, a typical lake in the semi-arid cold area of China, to investigate the diurnal variation of the ice surface albedo. Observations showed that the diurnal variations of the ice surface albedo exhibit bimodal characteristics with peaks occurring after sunrise and before sunset. The curve of ice surface albedo with time is affected by weather conditions. The first peak occurs later on cloudy days compared with sunny days, whereas the second peak appears earlier on cloudy days. Four probability density distribution functions—Laplace, Gauss, Gumbel, and Cauchy—were combined linearly to model the daily variation of the lake ice albedo on a sunny day. The simulations of diurnal variation in the albedo during the period from sunrise to sunset with a solar altitude angle higher than 5° indicate that the Laplace combination is the optimal statistical model. The Laplace combination can not only describe the bimodal characteristic of the diurnal albedo cycle when the solar altitude angle is higher than 5°, but also reflect the U-shaped distribution of the diurnal albedo as the solar altitude angle exceeds 15°. The scale of the model is about half the length of the day, and the position of the two peaks is closely related to the moment of sunrise, which reflects the asymmetry of the two peaks of the ice surface albedo. This study provides a basis for the development of parameterization schemes of diurnal variation of lake ice albedo in semi-arid cold regions.
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3

Guo, Yinglian, Jisong Sun, Guirong Xu, Zhiming Zhou, and Jizhu Wang. "Influence of Underlying Surface on Distribution of Hourly Heavy Rainfall over the Middle Yangtze River Valley." Advances in Meteorology 2022 (December 21, 2022): 1–14. http://dx.doi.org/10.1155/2022/9696174.

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The variation of boundary layer circulation caused by the influence of complex underlying surface is one of the reasons why it is difficult to forecast hourly heavy rainfall (HHR) in the middle Yangtze River Valley (YRV). Based on the statistics of high-resolution observation data, it is found that the low resolution data underestimate the frequency of HHR in the mountain that are between the twain-lake basins in the middle YRV (TLB-YRV). The HHR frequency of mountainous area in the TLB-YRV is much higher than that of Dongting Lake on its left and is equivalent to the HHR frequency of Poyang Lake on its right. The hourly reanalysis data of ERA5 were used to study the variation of boundary layer circulation when HHR occurred. It can be found that the boundary layer circulation corresponding to different underlying surfaces changed under the influence of the weather system. Firstly, the strengthening of the weather system in the early morning resulted in the strengthening of the southwest low-level air flow, which intensified the uplift of the windward slope air flow on the west and south slopes of the mountainous areas in the TLB-YRV. As a result, the sunrise HHR gradually increases from the foot of the mountain. The high-frequency HHR period of sunrise occurs when the supergeostrophic effect is weakened, the low-level vorticity and frontal forcing are strengthened, and the water vapor flux convergence begins to weaken. Secondly, the high-frequency HHR period of the sunset is caused by stronger local uplift and more unstable atmospheric stratification, but the enhanced local uplift is caused by the coupling of the terrain forcing of the underlying surface and the enhanced northern subgeostrophic flow, which causes the HHR to start closer to the mountain top at sunset than at sunrise.
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4

Amyot, Marc, David RS Lean, Laurier Poissant, and Marie-Renée Doyon. "Distribution and transformation of elemental mercury in the St. Lawrence River and Lake Ontario." Canadian Journal of Fisheries and Aquatic Sciences 57, S1 (March 14, 2000): 155–63. http://dx.doi.org/10.1139/f99-248.

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Elemental Hg (Hg0) is a volatile species that is responsible for water-to-air transfer of Hg in Lake Ontario and the St. Lawrence River. We conducted two cruises in 1998 to identify spatial and temporal patterns in Hg0 levels in these systems and performed field and laboratory experiments on redox transformations of Hg. Elemental Hg concentrations were higher in Lake Ontario than in the St. Lawrence River. At stations in Lake Ontario, Hg0 levels were higher at the bottom of the water column than at the surface, whereas they were homogeneous throughout the water column of the river. Elemental Hg concentrations were generally higher in July than in September and, in contrast with experiments on inland lakes, were relatively constant during the day except for a narrow peak at sunrise. Field and laboratory experiments showed that photoreduction of Hg(II) in St. Lawrence River water was substrate limited and was influenced by visible and ultraviolet radiation. Pseudo first-order kinetics best described photoreduction, with k values between 1 and 2·h-1.
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5

Levy, I., P. A. Makar, D. Sills, J. Zhang, K. L. Hayden, C. Mihele, J. Narayan, M. D. Moran, S. Sjostedt, and J. Brook. "Unraveling the complex local-scale flows influencing ozone patterns in the southern Great Lakes of North America." Atmospheric Chemistry and Physics Discussions 10, no. 8 (August 23, 2010): 19763–810. http://dx.doi.org/10.5194/acpd-10-19763-2010.

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Abstract. This study examines the complexity of various processes influencing summertime ozone levels in the southern Great Lakes region of North America. Results from the Border Air Quality and Meteorology (BAQS-Met) field campaign in the summer of 2007 are examined with respect to land-lake differences and local meteorology using a large array of ground-based measurements, aircraft data and simulation results from a high resolution (2.5 km) regional air-quality model, AURAMS. Analyses of average ozone mixing ratio from the entire BAQS-Met intensive campaign period support previous findings that ozone levels are higher over the southern Great Lakes than over the adjacent land. However, there is great heterogeneity in the spatial distribution of surface ozone over the lakes, particularly over Lake Erie during the day, with higher levels located over the southwestern end of the lake. Results suggest that some of these increased ozone levels are due to local emission sources in large nearby urban centers. The land-lake differences in ozone mixing ratios are most pronounced during the night in a shallow inversion layer of about 200 m above the surface. After sunrise, these differences have a limited effect on the total mass of ozone over the lakes during the day time, though they may cause elevated ozone levels in the lake breeze air. A large reservoir layer of ozone is predicted by the AURAMS model over Lake Erie at night, centered between 600–1000 m above ground and extending into the land over Cleveland. The model also predicts a vertical circulation during the day with an updraft over Detroit-Windsor and downdraft over Lake St. Clair, which transports ozone up to 1500 m above ground and results in high ozone over the lake. Oscillations in ground level ozone mixing ratios were observed on several nights and several ground monitoring sites, with amplitudes of up to 40 ppbv and time periods of 15–40 min.
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Levy, I., P. A. Makar, D. Sills, J. Zhang, K. L. Hayden, C. Mihele, J. Narayan, M. D. Moran, S. Sjostedt, and J. Brook. "Unraveling the complex local-scale flows influencing ozone patterns in the southern Great Lakes of North America." Atmospheric Chemistry and Physics 10, no. 22 (November 22, 2010): 10895–915. http://dx.doi.org/10.5194/acp-10-10895-2010.

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Abstract. This study examines the complexity of various processes influencing summertime ozone levels in the southern Great Lakes region of North America. Results from the Border Air Quality and Meteorology (BAQS-Met) field campaign in the summer of 2007 are examined with respect to land-lake differences and local meteorology using a large array of ground-based measurements, aircraft data, and simulation results from a high resolution (2.5 km) regional air-quality model, AURAMS. Analyses of average ozone mixing ratio from the entire BAQS-Met intensive campaign period support previous findings that ozone levels are higher over the southern Great Lakes than over the adjacent land. However, there is great heterogeneity in the spatial distribution of surface ozone over the lakes, particularly over Lake Erie during the day, with higher levels located over the southwestern end of the lake. Model results suggest that some of these increased ozone levels are due to local emission sources in large nearby urban centers. While an ozone reservoir layer is predicted by the AURAMS model over Lake Erie at night, the land-lake differences in ozone mixing ratios are most pronounced during the night in a shallow inversion layer of about 200 m above the surface. After sunrise, these differences have a limited effect on the total mass of ozone over the lakes and land during the day, though they do cause elevated ozone levels in the lake-breeze air in some locations. The model also predicts a mean vertical circulation during the day with an updraft over Detroit-Windsor and downdraft over Lake St. Clair, which transports ozone up to 1500 m above ground and results in high ozone over the lake. Oscillations in ground-level ozone mixing ratios were observed on several nights and at several ground monitoring sites, with amplitudes of up to 40 ppbv and time periods of 15–40 min. Several possible mechanisms for these oscillations are discussed, but a complete understanding of their causes is not possible given current data and knowledge.
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7

Ghan, David, J. D. McPhail, and K. D. Hyatt. "The temporal-spatial pattern of vertical migration by the freshwater copepod Skistodiaptomus oregonensis relative to predation risk." Canadian Journal of Fisheries and Aquatic Sciences 55, no. 6 (June 1, 1998): 1350–63. http://dx.doi.org/10.1139/f98-027.

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Skistodiaptomus oregonensis vertical migration in Kennedy Lake and Paxton Lake may be an adaptation to avoid predation by threespine stickleback (Gasterosteus aculeatus). In Kennedy Lake, juvenile sockeye salmon (Oncorhynchus nerka) and the mysid Neomysis mercedis are also predators that potentially drive the vertical migration. A corollary of the hypothesis that predation selects for vertical migration is that the extent and timing of the vertical migration decreases predation risk. This corollary is tested for each of the potential predators. Laboratory experiments indicate that stickleback feeding rate decreases below 1.6 µE ·s-1 ·m-2. In Kennedy and Paxton lakes, S. oregonensis occupied depths below this light intensity during the day. Furthermore, as S. oregonensis ascended at dusk and descended at dawn, they remained within light intensities that reduced stickleback predation rate. In Kennedy Lake, hydroacoustic data coupled with information in the literature on feeding behaviour of juvenile sockeye indicate that this species move to surface waters to feed before sunrise and after sunset. Vertically migrating S. oregonensis are near the surface during the twilight feeding periods of juvenile sockeye. The timing of S. oregonensis vertical migration also does not reduce the time it is in contact with the predator N. mercedis.
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8

Gussoni, Carlos Otávio A., and André C. Guaraldo. "Comportamento de forrageamento do pernilongo-de-costas-brancas, Himantopus melanurus (Vieillot, 1817) (Aves: Recurvirostridae) em Santa Gertrudes, SP, Brasil." Lundiana: International Journal of Biodiversity 7, no. 2 (June 28, 2007): 149–50. http://dx.doi.org/10.35699/2675-5327.2006.23155.

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The foraging behavior of two White-backed stilts (Himantopus melanurus) was studied in a lake at the municipality of Santa Gertrudes, state of São Paulo, Brazil. The foraging strategies observed were classified in two categories: pluging (65.8% of total maneuvers) and pecking (34.3%). Only in 26.8% of the foraging maneuvers the individuals captured preys (72.9% by plunging and 27.1% by pecking). When comparing both strategies, plunging was successful 29.7% of the times, but pecking only 21.2%. At the study site, individuals foraged only up to 20 m away from the lake margin. The foraging area exploited by the White-backed stilts was estimated in about 720 m2. Foraging activities lasted since before sunrise until after sunset. Keywords: White-backed stilt, foraging behavior, plunging, pecking.
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9

Silsbe, Greg M., Ralph E. H. Smith, and Michael R. Twiss. "Quantum efficiency of phytoplankton photochemistry measured continuously across gradients of nutrients and biomass in Lake Erie (Canada and USA) is strongly regulated by light but not by nutrient deficiency." Canadian Journal of Fisheries and Aquatic Sciences 72, no. 5 (May 2015): 651–60. http://dx.doi.org/10.1139/cjfas-2014-0365.

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Unattended sensor networks are a cost-effective strategy to enhance the resolution of environmental datasets and are required to understand how large aquatic ecosystems respond to complex stressors (e.g., climate change). We made unattended and continuous measurements of the quantum yield of photosystem II ([Formula: see text]) photochemistry in the surface mixed layer of Lake Erie during three lake-wide cruises to observe how phytoplankton physiology varied across nutrient and taxonomic gradients. Three prominent diel [Formula: see text] patterns were noted. The diel maximum consistently occurred at sunrise or sunset, nocturnal measurements were consistently lower than diel maxima, and daytime values were strongly diminished by nonphotochemical quenching. The diurnal pattern was modeled as a function of irradiance to a mean accuracy of 0.03 to 0.04. Contrary to previously published reports in Lake Erie, [Formula: see text] was largely insensitive to indices of nutrient deficiency through space and time. This finding was consistent with much recent literature about [Formula: see text] and suggests that Lake Erie phytoplankton, like many others, can tune their photosynthetic machinery to maintain relatively high efficiency of photochemistry in photosystem II even when deficient in phosphorus or nitrogen.
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10

Chrust, Morgan F., C. David Whiteman, and Sebastian W. Hoch. "Observations of Thermally Driven Wind Jets at the Exit of Weber Canyon, Utah." Journal of Applied Meteorology and Climatology 52, no. 5 (May 2013): 1187–200. http://dx.doi.org/10.1175/jamc-d-12-0221.1.

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AbstractThermally driven valley-exit jets were investigated at Utah’s Weber Canyon, a main tributary of the Great Salt Lake basin. An intensive measurement campaign during July–September 2010 supplemented longer-term measurements to characterize the wind and temperature structure in the vicinity of the canyon exit. Exit jets at Weber Canyon are most frequent in late summer or early fall. Strong low-level-wind jets formed at the canyon exit on 75 of 90 nights (83%) during the measurement campaign, with the best-developed winds forming during synoptically undisturbed, clear-sky periods. Winds inside the canyon consisted of a weak down-valley flow layer that occupied most of the 1000-m depth of the canyon. The flow was observed to descend, thin, and accelerate at the valley exit, producing winds that were typically 2.5 times as strong but much more shallow than those inside the canyon. Maximum nighttime jet-axis wind speeds of 15–20 m s−1 are typically found about 80–120 m above the ground at the canyon exit on clear undisturbed nights in the late summer and fall. The jets form 1–3 h after sunset, approach a near-steady state during the late night, and continue until 5–6 h after sunrise, although slowly losing speed after sunrise. The jet is a local modification at the canyon exit of the thermally driven down-valley flow. Its continuation after sunrise is thought to be caused by the nighttime buildup and persistence of a cold-air pool in the Morgan Basin at the east end of the canyon. The potential for utilizing the exit jet for wind power generation is discussed.
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Books on the topic "Lake Sunrise"

1

Timmers, Ginny. Sunrise Lake. Stargazer Publishing, 2004.

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Natelborg, Don. Sunrise at Marston's Lake. Independently Published, 2020.

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Engstrom, Alan. Sunrise at Marston's Lake. Independently Published, 2020.

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Feehan, Christine. Murder at Sunrise Lake. Little, Brown Book Group Limited, 2022.

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Feehan, Christine. Murder at Sunrise Lake. Thorndike Press Large Print, 2021.

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Feehan, Christine. Murder at Sunrise Lake. Berkley, 2021.

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Feehan, Christine. Murder at Sunrise Lake. Penguin Publishing Group, 2022.

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Sperry, An. Sunrise Honeymoons: Lake Geneva Love Poems. Independently Published, 2020.

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Bardino, Sarah. Notebear: Lake Atitlan Forest Sunrise Journal. Independently Published, 2019.

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Natelborg, Don. Sunrise at Marston's Lake: Large Print Edition. Independently Published, 2020.

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Book chapters on the topic "Lake Sunrise"

1

Bergstrom, Janet. "Murnau’s Sunrise: In-Camera Effects and Effects Specialists." In Special Effects on the Screen. Nieuwe Prinsengracht 89 1018 VR Amsterdam Nederland: Amsterdam University Press, 2022. http://dx.doi.org/10.5117/9789462980730_ch12.

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During the late 1920s, cinematographers in the US insisted that they should supervise outside specialists. An unforgettable “special effects” shot in Sunrise was photographed according to the needs of outside specialist Frank Williams’s patented process and his own lab. Understanding the Williams shot encourages us to see other unusual technical processes throughout Sunrise as they served Murnau’s drama rather than innovation for its own sake. Studying the achievement and function of specific shots in Sunrise leads to the larger debate about creative technical-aesthetic control that is similar to modern-day arguments about who should determine the final look of a film: digital postproduction specialists or the cinematographer, production designer, and director working together.
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Franklin, Peter. "Sunsets, Sunrises, and Decadent Oceanics." In Reclaiming Late-Romantic Music, 53–81. University of California Press, 2014. http://dx.doi.org/10.1525/california/9780520280397.003.0003.

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Marcus, Laura. "F. W. Murnau’s Sunrise." In A Modernist Cinema, 108–25. Oxford University Press, 2021. http://dx.doi.org/10.1093/oso/9780199379453.003.0007.

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In 1926, the German film director F. W. Murnau (born F. W. Plumpe) traveled to Hollywood to make his first American film, Sunrise (1927), for Fox. The modernism of Sunrise inheres in the contrasts it sets up between the country and the city, pastoralism and the modern urban, and this chapter explores it in part as a modernist city film. This aspect is linked to the film’s status as a late silent film: Sunrise reaches out toward the articulation of language and sound, intertwining these with the image of the modern city. Silence is placed on the side of the rural and the pictorial, sound on the side of the urban and dynamic. The two women in the film (representing country and city) occupy the poles of these oppositions in what may appear a simple allegory of good and evil, but the film in fact articulates a more complex and ambivalent attitude toward the old world and the new.
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"3. Sunsets, Sunrises, and Decadent Oceanics." In Reclaiming Late-Romantic Music, 53–81. Berkeley: University of California Press, 2019. http://dx.doi.org/10.1525/9780520958036-005.

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Robin, Cynthia. "Ordinary People and East–West Symbolism." In Maya E Groups. University Press of Florida, 2017. http://dx.doi.org/10.5744/florida/9780813054353.003.0011.

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This chapter explores the possibility that east-west symbolism is an enduring aspect of Maya culture that was initially developed in farmers' community centers and homes and later appropriated by society's nobility and encoded in hieroglyphic texts and images and enshrined in the monuments of major civic-centers. This chapter explores these ideas through the analysis of the central religious complex at the ancient Maya farming community of Chan in Belize. Chan’s central religious complex follows a construction sequence reminiscent of other E Groups, particularly the Cenote-style E Group, across the Maya area. It begins initially as a linear bedrock outcrop upon which architecture construction begins in the Late Preclassic (350 BCE-CE 0). The distance between the east and west structures of Chan’s central religious complex was always maintained throughout its architectural reconstruction history. If one of the functions of the west structure was viewing sunrise over the tripartite east structure, then maintaining a relative distance between the two structures could have been integral in maintaining lines of sight. Chan’s central religious complex was also a location for the burial of venerated ancestors, and those individuals from the community selected for veneration included men, women, and children.
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Das, Sankar. "Role of Government to Boost up the Food Processing Industry- A Study with Reference to Covid19 Pandemic." In Sustainable Strategies for Economic Growth and Decent Work: New Normal, 170–78. Lincoln University College, Malaysia, 2022. http://dx.doi.org/10.31674/book.2022sseg.020.

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Micro, Small and Medium Enterprises (MSME) are facing several problems due to the pandemic. The Food Processing Industry (FPI) is considered the sunrise sector of MSME. FPI establishes linkages and synergy amongst the primary, secondary, and tertiary sectors. More than 40000 registered and 25 lakh unregistered food processing units exist in India, in which 7 million labours are engaged. Due to the sudden lockdown, huge quantities of raw materials and finished products have started to rot, and many units have been forced to shut down, and a huge number of workers in this industry have lost their jobs. The industry needed strong Government intervention to survive this crisis. The study has tried to focus on the impact of lockdown on FPI and the role of the government in boosting this industry during the current crisis period. The study is based on secondary data. The Central Government has tried to boost the industry by announcing a financial package of Rs. 10,000 crores for the establishment of micro food enterprises, changing the definition of MSME and providing relaxation in tax and other laws. A positive approach by the Central Government will definitely support the food processing industry to turn around under this critical situation.
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