Добірка наукової літератури з теми "Hawaiki"

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Статті в журналах з теми "Hawaiki"

1

Brockway, Robert W. "The whence of Hawaiki." Studies in Religion/Sciences Religieuses 16, no. 2 (June 1987): 221–30. http://dx.doi.org/10.1177/000842988701600208.

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Kimball, Linda Amy, and Margaret Orbell. "Hawaiki: A New Approach to Maori Tradition." Journal of American Folklore 101, no. 399 (January 1988): 120. http://dx.doi.org/10.2307/540282.

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Terrell, John Edward, Patrick Vinton Kirch, and Roger C. Green. "Hawaiki, Ancestral Polynesia: An Essay in Historical Anthropology." Pacific Affairs 75, no. 2 (2002): 342. http://dx.doi.org/10.2307/4127236.

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Metzgar, Eric. "Hawaiki Rising: Hōkūle‘a, Nainoa Thompson, and the Hawaiian Renaissance." Journal of Pacific History 54, no. 3 (April 29, 2019): 431–32. http://dx.doi.org/10.1080/00223344.2019.1603620.

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Adds, P. "Long-distance prehistoric two-way voyaging: the case for Aotearoa and Hawaiki." Journal of the Royal Society of New Zealand 42, no. 2 (June 2012): 99–103. http://dx.doi.org/10.1080/03036758.2012.677456.

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Kaeppler, Adrienne L. "Hawaiki, Ancestral Polynesia: An Essay in Historical Anthropology. Patrick Vinton Kirch , Roger C. Green." Journal of Anthropological Research 58, no. 4 (December 2002): 565–66. http://dx.doi.org/10.1086/jar.58.4.3630689.

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Di Piazza, Anne. "Patrick Vinton Kirch & Robert C. Green, Hawaiki, Ancestral Polynesia. An Essay in Historical Anthropology." L'Homme, no. 163 (June 21, 2002): 309–10. http://dx.doi.org/10.4000/lhomme.12771.

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Drager, Katie. "Pidgin and Hawai‘i English: An overview." International Journal of Language, Translation and Intercultural Communication 1 (January 1, 2012): 61. http://dx.doi.org/10.12681/ijltic.10.

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<strong><strong></strong></strong><p align="LEFT">T<span style="font-family: DejaVuSerifCondensed; font-size: small;"><span style="font-family: DejaVuSerifCondensed; font-size: small;">oday, most people from Hawai‘i speak Pidgin, Hawai‘i English, or both. This </span></span>paper presents a brief discussion of the history of both the creole (called Pidgin or Hawaii Creole) and the variety of English spoken in Hawai‘i referred to as Hawai‘i English. The creation of Pidgin and the prevalence of English in Hawai‘i have a complex history closely tied with various sociohistorical events in the islands, and the social hegemony established during the plantation days still persists today. While Pidgin is stigmatized and is deemed inappropriate for use in formal domains, it has important social functions, and the infl uence from diff erent languages is viewed as representative of the ethnic diversity found in the islands. This paper treats Pidgin and Hawaii English as independent from one another while commenting on some of the linguistic forms that are found in both. Lexical items, phonological forms,and syntactic structures of Pidgin and Hawai‘i English are presented alongside a discussion of language attitudes and ideologies. Recent work that attempts to address the negative attitudes toward Pidgin is also discussed.</p>
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KIM, ALICE, and NICOLE C. LAUTZE. "TOURISTS PLAY WITH LAVA AND VOLCANIC HEAT: KĪLAUEA VOLCANO’S EARLY CONTRIBUTIONS TO HAWAI‘I’S TOURISM INDUSTRY." Earth Sciences History 40, no. 1 (January 1, 2021): 244–60. http://dx.doi.org/10.17704/1944-6187-40.1.244.

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ABSTRACT Kīlauea Volcano has attracted visitors to Hawai‘i throughout the history of Hawai‘i’s tourism industry. From the 1870s to the 1910s, Kīlauea offered the experience of using volcanic heat and molten lava to cook food, melt postcards onto cavern walls, enflame items, and obtain souvenirs including scorched postcards, rocks, olivine, and Pele’s hair. Writers shared their experiences in publications, and traveling presentations showed American audiences images of visitors scorching postcards at Kīlauea. Marketing campaigns on the U.S. Mainland promoted Hawai‘i as a tourist destination and promoted cooking with Kīlauea’s heat. In 1907, U.S. Congressmen toured Kīlauea Caldera, ate dinner cooked with Kīlauea’s heat, and learned about Kīlauea’s geodiversity. These experiences likely influenced Congress to establish the Kīlauea, Haleakalā, and Mauna Loa Volcanoes as the Hawaii National Park (now known as the Hawai‘i Volcanoes National Park). Today, the U.S. National Park Service maintains the Hawai‘i Volcanoes National Park, and it offers geological, biological, and cultural resources for recreation and education. For destination marketing, Kīlauea provided Hawai‘i a comparative advantage for tourism.
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BABA, KEIJI. "Babamunida debrae, a new species of squat lobster (Crustacea: Anomura: Galatheoidea: Munididae) from the Hawaiian Islands." Zootaxa 2812, no. 1 (April 8, 2011): 21. http://dx.doi.org/10.11646/zootaxa.2812.1.2.

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A new species of squat lobster, Babamunida debrae, was found in shallow waters of the west coast of Hawai‘i. It is readily distinguished from all the other species of the genus by the presence of a pair of spines on the second abdominal tergite. Babamunida debrae is the second species of the genus from Hawaii and seventh species of the genus from the Indo-Pacific.
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Дисертації з теми "Hawaiki"

1

Ayala, Monica. "Climate Variability from 1980 to 2018 and its Effect on Wind Directions, Wind Speeds, and Vog Dispersal in Hawaii." Digital Commons @ East Tennessee State University, 2020. https://dc.etsu.edu/etd/3776.

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Wind patterns in the Pacific Ocean fluctuate seasonally, annually, and decadally, resulting in changes in the dispersal of volcanic smog (vog) across the Hawaiian Islands. A variety of synoptic-scale weather patterns can affect the Islands, creating variability in the direction and intensity of wind patterns. Recent changes in wind profiles were analyzed to identify possible patterns that could influence and increase the dispersion of vog over time on Hawai’i Island and the other Hawaiian Islands to the northwest. Historically, Northeast Trade Winds prevailed for much of the year, shifting vog into the Pacific Ocean southwest of Hawaii and away from the state’s principal population centers, but Northeast Trade Winds have shown a 20+% reduction over the past several decades. An increase in the southerly source of prevailing wind increased the frequency and intensity of vog and its impacts on the environment and health and well-being of people across the Islands.
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Lemarié, Jérémy. "Genèse d’un système global surf : regards comparés des Hawai‘i à la Californie : traditions, villes, tourismes, et subcultures (1778–2016)." Thesis, Paris 10, 2016. http://www.theses.fr/2016PA100048/document.

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En traitant de l’histoire coloniale des Hawai‘i et de la Californie à partir de 1778, cette thèse étudie de la transformation de la coutume hawaïenne he‘e nalu en un système surf mondial. L’analyse se demande s’il y a eu rupture ou continuité du surf hawaïen au XIXe siècle, et quelles ont été les modalités de sa diffusion en tant que système mondial surf au XXIe siècle. Pour répondre à ce problème, ce travail a retenu trois méthodes d’investigations : une analyse comparative des journaux de bords des voyageurs vers l’archipel des Hawai‘i avec la presse hawaïenne au XIXe siècle ; la conduite de cinquante entretiens semi-directifs, pour saisir les enjeux de l’appropriation californienne du surf après 1945 ; et une observation participante multi-site de trente mois aux Hawai‘i et en Californie, entre 2009 et 2016, afin de dégager les modalités contemporaines de l’historicisation du surf. Au final, trois conclusions principales ont été dégagées à partir de ces données. D’abord, l’introduction des Hawai‘i dans le système monde au XIXe siècle a dynamisé la naissance d’une identité nationale autochtone, qui a réaffirmé les coutumes traditionnelles, comme le surf. Ensuite, avec l’avènement du tourisme balnéaire au XXe siècle, les Hawai‘i se sont imposés comme un modèle touristique, reposant sur la mise en scène et l’appropriation occidentale du surf. À cet égard, Waikīkī est un cas d’école, et son schéma de développement s’est reproduit en Californie, comme à Huntington Beach. Enfin, à partir des années 1950, le surf s’est exporté dans le monde grâce à l’émergence de sa subculture et de son sport professionnel, aux médias de masse, et à la démocratisation du tourisme balnéaire
Dealing with the colonial history of Hawai‘i and California from 1778, this dissertation focus on the transformation of the Hawaiian custom he‘e nalu into a global surf system. This analysis asks if there a break or a continuity of Hawaiian surfing in the 19th century, and what are the terms and conditions of its diffusion as a global surf system in the 21st century. Three investigating methods have been applied: an analysis of traveling literature in Hawai‘i, compared with a study of Hawaiian newspapers in the 19th century ; a recording of fifty semi-directed interviews to grasp issues related to appropriating surfing in California after 1945 ; and a multi-sited participant observation for thirty months in Hawai‘i and California, between 2009 and 2016, to found out about the contemporary historicization of surfing. Three main conclusions emerged from this data analysis. First, the introduction of Hawai‘i in the world system in the 19th century fostered the birth of a Hawaiian national identity, that reaffirmed traditional customs, such as surfing. Then, with the advent of seaside tourism in the 20th century, Hawai‘i became a touristic model, based on staging surfing and its appropriation by the West. To this regard, Waikīkī is a popular case study, and its development pattern has been reproduced in Californian cities, such as Huntington Beach. Eventually, from the 1950s, surfing has been exported to the world, thanks to the growth of its subculture and professional sport, mass media, and the democratization of seaside tourism
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Garrison, Geoffrey Hjorth. "Holocene sedimentary and aquatic biogeochemical responses reflected in Ordy Pond, Oahʻu, Hawai'i, and, contemporary modeling of submarine groundwater discharge in Kahana Bay, Oahʻu, Hawaiʻi". Thesis, University of Hawaii at Manoa, 2002. http://hdl.handle.net/10125/3021.

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This dissertation explores aquatic geochemistry in two settings on O'ahu. Ordy Pond biogeochemistry responds rapidly to environmental changes, while Kahana Bay is influenced by significant groundwater and surface water influx and mixing with coastal ocean water. Thus, Ordy Pond is a better tool for studying Oahu's paleoenvironments, and Kahana Bay demonstrates the applicability of natural chemical tracers to quantify submarine groundwater discharge (SGD). Work in Ordy Pond consisted of modern water column and particulate production time-series analyses, and sediment core study. Air temperature changes appeared to control the seasonal water chemistry. When the pond was thermally stratified in the spring/summer, epilimnion primary productivity increased dramatically as indicated by dissolved O2, dissolved inorganic carbon, S13CDIC, and particulate production rates. Once the density gradient waned, the anoxic hypolimnion mixed with the epilimnion, organic matter productivity fell, and surface waters became suboxic to anoxic. Primary productivity is believed to have been controlled by the availability of sunlight; the longer daily photoperiod during stratification resulted in greater organic matter production, while greater mixing in winter reduced the photoperiod, increased phytoplankton respiration, and reduced organic matter production. The carbonate mineral flux increased during elevated primary productivity due to increased carbonate mineral saturation states. Modern particulate production closely reflected the water chemistry, and the biogeochemical processes in the modern pond were used to interpret the Holocene environmental history of the area through analysis of pond sediments. The sediments revealed three dramatic paleoenvironmental events: 1) the most recent post-glacial sea level rise around Oʻahu ~ 9.7 kya; 2) sea level fall ~1 kya following Oahu's mid Holocene Sea level high stand; and 3) Western human contact with O'ahu and the introduction of plantation-scale agriculture. Finally, in a separate study of the submarine ground water discharge to Oahu's coastal waters, Kahana Bay was found to experience a much greater exchange with the surrounding environment than Ordy Pound. Total SGD in Kahana Bay is significant (90 x 106 L d-1), providing 16% as much terrestrial water, five times as much phosphorus, and two times as much nitrogen as surface water runoff.
Thesis (Ph. D.)--University of Hawaii at Manoa, 2002.
Includes bibliographical references.
Mode of access: World Wide Web.
Also available by subscription via World Wide Web
1 v. (various pagings), leaves, bound ill., maps 29 cm
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Affandy, Gabriel, Donald Bridges, Quinn Daniels, Drew Janicek, Julia Martin, Edward Poling, Jordan Schmalz, et al. "HAWAII ALGAL BIOFUEL." Monterey, California. Naval Postgraduate School, 2013. http://hdl.handle.net/10945/32891.

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This report investigates the feasibility and affordability of producing algae-derived biofuel in Hawaii for military aviation. The authors evaluated methods for cultivation of algae, investigated the processes necessary to locally refine bio-oil into bio-kerosene, researched the environmental impacts of cultivation and refinement facilities in Hawaii, and studied the resultant cost per gallon of bio-kerosene production. Based on the current state of technology and the proposed system of systems architecture, this report estimates that bio-kerosene can be produced for $8.00 - 22.87/gal, indicating that although this system is technically feasible, it is unlikely to be affordable at current fuel prices without ongoing subsidy or further technical innovation.
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LaBarge, Andrea L. "Hawaii government's role in Japanese ownership of Hawaii hotels, 1970-1990." Thesis, University of Hawaii at Manoa, 2002. http://proquest.umi.com/pqdweb?index=0&did=765044491&SrchMode=1&sid=8&Fmt=2&VInst=PROD&VType=PQD&RQT=309&VName=PQD&TS=1208551486&clientId=23440.

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Sato, Alvin H. "Pregnancy intendedness in Hawaiʻi: findings from the Hawaiʻi pregnancy risk assessment monitoring system, 1999". Thesis, University of Hawaii at Manoa, 2002. http://hdl.handle.net/10125/3036.

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The purpose of this study was to investigate the relationship between unintended pregnancies and demographic factors in Hawaiʻi, and to investigate the relationship between unintended pregnancies and violence in Hawaiʻi. This study used an observational, cross-sectional probability sample drawn women from June 1999 through December 1999. Women who were selected received Hawaiʻi Pregnancy Risk Assessment Monitoring System (PRAMS) questionnaires generated from the Hawaiʻi State Department of Health. The main variables from the PRAMS questionnaire investigated in the study were maternal pregnancy intendedness, physical abuse 12 months before pregnancy and physical violence during pregnancy. Controlling variables investigated were maternal age, maternal education, marital status, geographical location, maternal ethnicity, parity status, Quest status, source of prenatal care, and contraceptive use. This dissertation supports the proposed ecological conceptual framework for understanding unintended pregnancies and physical violence during and around the time of pregnancy. Using this model, it could be hypothesized that women with unintended pregnancies tend to live in less stable environments and therefore unintended pregnancies and physical violence could be part of the same social problems. In general, bivariate analysis showed unintended pregnancies were significantly associated with SES factors. However, controlling for all variables in the model, only maternal age, parity status, marital status and contraceptive use were significantly associated with unintended pregnancies. Crude odds ratio showed a significant association between maternal pregnancy intendedness and physical abuse twelve months prior to pregnancy. However, when controlling for all variables in the study model proved to be not significant. A better understanding of unintended pregnancies and physical abuse around the time of pregnancies would help professionals in Hawaiʻi to screen for at risk individuals.
Thesis (Ph. D.)--University of Hawaii at Manoa, 20##.
Mode of access: World Wide Web.
Includes bibliographical references (leaves 110-115).
Electronic reproduction.
Also available by subscription via World Wide Web
xiii, 115 leaves, bound ill. 29 cm
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Luangphinith, Seri Inthava Kauʻikealaula. "Reading the literature of Hawaiʻi /". view abstract or download file of text, 2000. http://wwwlib.umi.com/cr/uoregon/fullcit?p9986746.

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Thesis (Ph. D.)--University of Oregon, 2000.
Typescript. Includes vita and abstract. Includes bibliographical references (leaves 219-232). Also available for download via the World Wide Web; free to University of Oregon users.
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Eversole, Dolan. "Large-Scale Beach Change: Kaanapali, Hawai'i." Thesis, University of Hawaii at Manoa, 2002. http://hdl.handle.net/10125/6946.

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Using monthly beach profile surveys and historical aerial photographs, the seasonal and long-term (48 year) beach morphology for Kaanapali Beach, Maui is described. By identifying the shoreline position in historical aerial photographs it is determined that the Kaanapali area is subject to long periods of mild erosion and accretion punctuated by severe erosional events related to short-period Kona storms and hurricane waves. Increased Central Pacific tropical cyclone activity of the late 1950's and early 1960's and Hurricane Iniki in 1992 are identified as contributing factors to the observed volume change during these periods. Between these erosional periods the Kaanapali shoreline is relatively stable characterized by light erosion to moderate accretion suggesting the recovery time may be on the order of roughly 20 years. Over the 48-year period 1949 to 1997, the Kaanapali and Honokowai cells have experienced a net sediment volume loss of 43,000 ±730 m3 and 30,700 ±630 m3 respectively for a total net volume loss of 73,700 ± 990 m3. The Kona storms and hurricanes of the early 1960's and 1992 collectively account for 136,000 m3 of sediment lost or approximately 62% of the gross volume change for the entire period, revealing the significant erosional effect of these storms. Recovery after each of these storms accounts for 73,900 m3 or approximately 33% of the gross volume change. A residual loss of 10,600 m3 representing 5% of the gross volume change is inferred as chronic erosion and may be a product of relative sea-level rise (RSLR). An increase in short-period southwesterly wave energy during these erosional periods is well documented and may have transported beach sediment further offshore than normal (beyond the reef) and is identified as a possible mechanism for long-term erosion in this area. The spatial distribution of historical shoreline movement suggests the majority of sediment transport occurs in the central portion of Kaanapali near Kekaa and Hanakoo Point and is driven by longshore rather than cross-shore transport. Surveyed beach profiles reveal a strong seasonal variability with net erosion in the summer and accretion in the winter with an along the shore-alternating pattern of erosion and accretion. 65% of the net volume change occurs south of Kekaa Point confirming the more dynamic nature of the southern (Kaanapali Cell). Net beach profile volume change from the mean suggests that June and January are the most dynamic months each with approximately 14% of the total volume change. We attribute the significant and rapid erosion and accretion events due to wave-induced longshore transport of sediment. Field observations of monthly beach sediment impoundment in the Kaanapali cell are examined and compared to three models that predict longshore sediment transport (LST). Beach profile results indicate sediment impoundment occurs seasonally with a nearly balanced longshore sediment transport system between profile 5 and 9. Longshore transport rates are derived from seasonal cumulative net volume change in the middle of Kaanapali Beach at profile 7. Cumulative net sediment transport rates are 29,379 m3/yr ±15% to the north and 22,358 m3/yr ± 6% to the south for summer and winter respectively, a net annual rate of 7,021 m3/yr ± 10% to the north and a gross annual rate of 51,736 m3/yr ± 2%. Predictive transport formulas such as CERC (1984), CERC (1991) and Kamphius (1991) predict net annual transport rates at 3 x 103 percent, 77 percent and 6 x 103 percent of the observed transport rates respectively. The presence of fringing reef significantly effects the ability of the LST models to accurately predict sediment transport. When applying the CERC (1984, 1991) and Kamphius (1991) formulas, the functional beach profile area available for sediment transport is assumed much larger than actually exists in Kaanapali because of the presence of a fringing reef that truncates a portion of the sandy profile area. The CERC (1984, 1991) and Kamphius (1991) formulas don't account for the presence of a reef system which may contribute to the models overestimate of longshore sediment transport as they assume the entire profile is mobile sediment. However the fact that the CERC (1991) model underestimates the observed transport implies that additional environmental parameters (such as wave height, direction and period) playa more substantial role than the influence of the reef in the model results. The CERC (1991) Genesis model is found to be superior in fitting the observed longshore transport at Kaanapali Beach. The success of the Genesis model is partly attributed to its' ability to account for short-term changes in near-shore parameters such as wave shoaling, refraction, bathymetry, antecedent conditions and several other shore face parameters not accounted for in the CERC (1984) or Kamphius (1991) formulas. The use of the CERC (1984) formula is prone to practical errors in its' application particularly in the use of the recommended "K" coefficient and wave averaging that may a significantly overestimate the LST. A better fit to the observed LST is achieved with the CERC (1984) if the K value is decreased by an order of magnitude from 0.77 to 0.07. The Kamphius (1991) formula is especially sensitive to extremes in wave period and tends to deviate from observed transport estimates for unusually high wave periods (this study) and approximates observations nicely in areas with low wave periods (Ping Wang et al. (1998). Many of the studied predictive LST formulas are prone to overestimate transport and thus their use requires a comprehensive understanding of the complexities and errors associated with employing them. Great care must be used when applying LST models in areas with significant hard bottom or shallow reefs that alter the beach profile shape. Due to these errors, the use of the CERC (1984) and Kamphius (1991) formulas are better suited as a qualitative interpretative tool of transport direction rather than magnitude.
ix, 62 leaves
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Engels, Mary S. "Holocene reef accretion: Southwest Molokai, Hawai'i." Thesis, University of Hawaii at Manoa, 2003. http://hdl.handle.net/10125/6999.

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Two reef systems off south Molokai, Hale O Lono and Hikauhi, show differences in modern ecosystem structure and Holocene accretion history that reflect the influence of wave-induced near-bed shear stresses on reef development in Hawaii. Both sites are exposed to similar impacts from southern, Kona, and trade wind swell, but differing wave impacts result from relative exposure to north swell. Analysis and dating of 10 cores from Hale O Lono reveal a back stepping reef ranging from ~8,100 cal yr BP (offshore) to ~4,800 cal yr BP (nearshore). A depauperate community of modern coral diminishes shoreward and seaward of~15 m depth due to wave energy, disrupted recruitment activities and physical abrasion. Evidence suggests a change from conditions conducive to accretion during the early Holocene to conditions detrimental to accretion in the late Holocene. Reef structure at Hikauhi, reconstructed from 14 cores, reveals a thick, rapidly accreting and young (maximum age ~900 cal yr BP) prograding reef. Modem live coral cover on this reef increases seaward with distance from the reef crest but terminates at a depth of ~20m where the reef ends in a large sand field. The primary limitation on vertical reef growth is accommodation space under wave base, not recruitment activities or energy conditions. This study suggests modem reef growth on the southwest comer of Molokai is controlled by wave-induced near-bed shear stress related to refracted North Pacific swell. Holocene accretion patterns here also reflect the influence of wave-induced near-bed shear stress from north swell. Other factors controlling Holocene reef accretion are relative sea-level and wave sheltering by Laau Point. Habitat suitable for reef accretion on the southwest shore of Molokai has shrunk throughout the Holocene.
ix, 62 leaves
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10

Gillmar, Emily S. T. 1978. "Toward a shifting inhabitation, Kaho'olawe, Hawaii." Thesis, Massachusetts Institute of Technology, 2005. http://hdl.handle.net/1721.1/30230.

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Thesis (M. Arch.)--Massachusetts Institute of Technology, Dept. of Architecture, 2005.
Includes bibliographical references (p. 74-75).
The island of Kaho'olawe is a desert island in the Romantic sense: it is unapproachable and unsettleable, yet always an object of desire. Waterless, used for military target practice, cleaned up, and being replanted, the island requires an architecture that acknowledges and aids the continual re-making of the site. This project is an infrastructure--physical and programmatic--for connection and access to Kaho'olawe; in certain locations, the infrastructure manifests itself as architectural gestures, shelters for people who come to the island. The infrastructure is for people and plants, inscribing continual change on different scales of time and space. The architecture consciously makes and records traces, and the traces in turn are remade by subsequent visitors and rearrangements of the architecture.
Emily S.T. Gillmar.
M.Arch.
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Книги з теми "Hawaiki"

1

Leaf, Joan M. Hawaiki 2000 B.C. to Hokianga. [Rawene, N.Z.]: J.M. Leaf, 1993.

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2

Hawaiki: A new approach to Maori tradition. Christchurch: University of Canterbury, 1985.

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3

Orbell, Margaret Rose. Hawaiki: A new approach to Maori tradition. Christchurch: Canterbury University Press, 1991.

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4

Curtis, Green Roger, ed. Hawaiki, ancestral Polynesia: An essay in historical anthropology. Cambridge: Cambridge University Press, 2001.

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5

Hawaitō honoruru = HAWAII IS. HONOLULU. Tōkyō: Jitsugyōnonihonsha, 2011.

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6

Yi, Chin-yŏng. Hawai: 17-18 ch'oesinp'an = Hawaii. Sŏul-si: RHK (Areich'i K'oria), 2017.

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7

The discovery of Aotearoa. Auckland, N.Z: Reed, 1998.

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8

Nilsen, Robert. Big island of Hawaiì: Including Hawaii Volcanoes National Park. 5th ed. Emeryville, Calif: Avalon Travel, 2003.

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9

Kurabu, Aroha, ed. Hawai kozure ryokō gaido: We are laughing in Hawaii. Tōkyō: Shōgakkan, 2000.

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10

Bo-ram, Kim, ред. Hawai yŏhaeng paeksŏ: Alloha nangmani sara innŭn chisang chʼŏnʼguk = Hawaii. Sŏul: Namu Chajŏn'gŏ, 2013.

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Частини книг з теми "Hawaiki"

1

Kwon, Brenda. "Hawai'i." In A Companion to the Regional Literatures of America, 458–76. Oxford, UK: Blackwell Publishing Ltd, 2007. http://dx.doi.org/10.1002/9780470999080.ch27.

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Fletcher, Charles H., and Eden J. Feirstein. "Hawaii." In Encyclopedia of the World's Coastal Landforms, 125–32. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-1-4020-8639-7_17.

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3

Treadwell, Timothy. "Hawaii." In The Patrick Moore Practical Astronomy Series, 83–97. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-50002-7_6.

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Watkins, Scott D., and Patrick L. Anderson. "Hawaii." In The State Economic Handbook 2010, 55–59. New York: Palgrave Macmillan US, 2009. http://dx.doi.org/10.1057/9780230102125_12.

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Watkins, Scott D., and Patrick L. Anderson. "Hawaii." In The State Economic Handbook 2008, 55–59. New York: Palgrave Macmillan US, 2007. http://dx.doi.org/10.1057/9780230607248_12.

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Berger, Sandra L. "Hawaii." In The Best Summer Programs for Teens, 118. 4th ed. New York: Routledge, 2021. http://dx.doi.org/10.4324/9781003238713-17.

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Watkins, Scott D., and Patrick L. Anderson. "Hawaii." In The State Economic Handbook 2009, 55–59. New York: Palgrave Macmillan US, 2008. http://dx.doi.org/10.1057/9780230614994_12.

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Coffman, Tom. "Reinventing Hawai‘i." In The Value of Hawaii, edited by Craig Howes and Jonathan K. K. Osorio, 9–14. Honolulu: University of Hawaii Press, 2017. http://dx.doi.org/10.1515/9780824860417-003.

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Campbell, J. F., R. M. Moberly, and H. F. Olson. "USA--Hawaii." In The GeoJournal Library, 443–51. Dordrecht: Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-2999-9_48.

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Heck, André. "USA-Hawaii." In StarGuides 2001, 751–55. Dordrecht: Springer Netherlands, 2001. http://dx.doi.org/10.1007/978-94-011-4349-3_108.

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Тези доповідей конференцій з теми "Hawaiki"

1

Ho Schar, Cathi, and Daniel S. Friedman. "The Politics of Repair in a Postcolonial Context: A Minor Case Study." In 2018 ACSA International Conference. ACSA Press, 2018. http://dx.doi.org/10.35483/acsa.intl.2018.51.

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The University of Hawai‘i at Mānoa is the flagship campus for the country’s most remote and westernmost state. It lies over two thousand nautical miles from the nearest continent, roughly in the center of the Pacific Ocean, the largest division of the world hydrosphere. Until 1893, Hawai’i was a sovereign kingdom. In 1959, the U.S. government annexed Hawaiʻi as the last and newest of its fifty states. This vivid context—Pacific, Asian, Hawaiian, American, postcolonial—constitutes both a geographical and cultural orientation. In view of these numerous, vivid conditions, our paper offers a single case study based on small projects underway at Mānoa, where the senior leadership of the university invited the newly established University of Hawai‘i Community Design Center to address the chronic disrepair of campus buildings and public spaces through low-cost, high-impact design interventions. The aim of these interventions is to improve perceived qualities of public space and campus character, which have suffered under the weight of the university’s half-billion dollar deferred maintenance backlog.
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2

Headley, Alexander, Benjamin Schenkman, Keith Olson, and Laurence Sombardier. "Least Cost Microgrid Resource Planning for the Natural Energy Laboratory of Hawaii Authority Research Park." In ASME 2021 15th International Conference on Energy Sustainability collocated with the ASME 2021 Heat Transfer Summer Conference. American Society of Mechanical Engineers, 2021. http://dx.doi.org/10.1115/es2021-63257.

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Abstract The Natural Energy Laboratory of Hawaii Authority’s (NELHA) campus on The Island of Hawai’i supplies resources for a number of renewable energy and aquaculture research projects. There is a growing interest at NELHA to convert the research campus to a 100% renewable, islanded microgrid to improve the resiliency of the campus for critical ocean water pumping loads and to limit the increase in the long-term cost of operations. Currently, the campus has solar array to cover some electricity needs but scaling up this system to fully meet the needs of the entire research campus will require significant changes and careful planning to minimize costs. This study will investigate least-cost solar and energy storage system sizes capable of meeting the needs of the campus. The campus is split into two major load centers that are electrically isolated and have different amounts of available land for solar installations. The value of adding an electrical transmission line if NELHA converts to a self-contained microgrid is explored by estimating the cost of resources for each load center individually and combined. Energy storage using lithium-ion and hydrogen-based technologies is investigated. For the hydrogen-based storage system, a variable efficiency and fixed efficiency representation of the electrolysis and fuel cell systems are used. Results using these two models show the importance of considering the changing performance of hydrogen systems for sizing algorithms.
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Headley, Alexander, Benjamin Schenkman, Keith Olson, and Laurence Sombardier. "Least Cost Microgrid Resource Planning for the Natural Energy Laboratory of Hawaii Authority Research Park." In ASME 2020 International Mechanical Engineering Congress and Exposition. American Society of Mechanical Engineers, 2020. http://dx.doi.org/10.1115/imece2020-23874.

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Анотація:
Abstract The Natural Energy Laboratory of Hawaii Authority’s (NELHA) campus on The Island of Hawai’i supplies resources for a number of renewable energy and aquaculture research projects. There is a growing interest at NELHA to convert the research campus to a 100% renewable, islanded microgrid to improve the resiliency of the campus for critical ocean water pumping loads and to limit the increase in the long-term cost of operations. Currently, the campus has solar array to cover some electricity needs but scaling up this system to fully meet the needs of the entire research campus will require significant changes and careful planning to minimize costs. This study will investigate least-cost solar and energy storage system sizes capable of meeting the needs of the campus. The campus is split into two major load centers that are electrically isolated and have different amounts of available land for solar installations. The value of adding an electrical transmission line if NELHA converts to a self-contained microgrid is explored by estimating the cost of resources for each load center individually and combined. Energy storage using lithium-ion and hydrogen-based technologies is investigated. For the hydrogen-based storage system, a variable efficiency and fixed efficiency representation of the electrolysis and fuel cell systems are used. Results using these two models show the importance of considering the changing performance of hydrogen systems for sizing algorithms.
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4

Dovermann, Karl Heinz. "Topology Hawaii." In Proceedings of the Topology Conference. WORLD SCIENTIFIC, 1992. http://dx.doi.org/10.1142/9789814538831.

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5

Sclafani, Anthony. "Analysis of Carbon Dioxide Emission Reductions From Energy Efficiency Upgrades in Consideration of Climate Change and Renewable Energy Policy Initiatives Using eQUEST." In ASME 2010 4th International Conference on Energy Sustainability. ASMEDC, 2010. http://dx.doi.org/10.1115/es2010-90143.

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In January 2008 the Governor of Hawaii announced the Hawaii Clean Energy Initiative; an initiative that aims to have at least 70 percent of Hawaii’s power come from clean energy by 2030 [4]. In July 2009, the Hawaii Department of Accounting and General Services awarded NORESCO, an energy service company, a $33.9M contract to improve the energy efficiency of 10 government buildings. The avoided utility cost of the energy and water savings from the improvements is the project funding mechanism. The energy savings realized by the project will reduce carbon dioxide emissions associated with utility power generation. However, as renewable energy becomes a larger portion of the utility generation profile through the Hawaii Clean Energy Initiative, the carbon dioxide emissions reductions from specific energy efficiency measures may erode over time. This work presents a method of analysis to quantify the carbon dioxide emissions reduction over the life of a project generated by energy efficiency upgrades that accounts for both the impact of policy initiatives and climate change using DOE-2/eQUEST. The analysis is based on the fact that HVAC energy usage will vary with climate changes and that carbon dioxide emission reductions will vary with both energy savings and the corresponding utility’s power generation portfolio. The energy savings related to HVAC system energy efficiency improvements are calculated over the life of a 20 year performance contract using a calibrated DOE-2/eQUEST model of an existing building that utilizes weather data adjusted to match the predictions of the Intergovernmental Panel on Climate Change. The carbon dioxide emissions reductions are calculated using the energy savings results and a projection of the implementation of the Hawaii Clean Energy Initiative. The emissions reductions are compared with other analysis methods and discussed to establish more refined expectations of the impact of energy efficiency projects in context with climate changes and policy initiatives.
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Garces, M. A., and W. Thelen. "Infrasound Monitoring in Hawaii." In Near-Surface Asia Pacific Conference, Waikoloa, Hawaii, 7-10 July 2015. Society of Exploration Geophysicists, Australian Society of Exploration Geophysicists, Chinese Geophysical Society, Korean Society of Earth and Exploration Geophysicists, and Society of Exploration Geophysicists of Japan, 2015. http://dx.doi.org/10.1190/nsapc2015-030.

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7

Curtis, George D. "Tsunami Mitigation in Hawaii." In Solutions to Coastal Disasters Congress 2008. Reston, VA: American Society of Civil Engineers, 2008. http://dx.doi.org/10.1061/40978(313)13.

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HAYWARD, THOMAS. "Spaceport Hawaii - Environmental issues." In Space Programs and Technologies Conference. Reston, Virigina: American Institute of Aeronautics and Astronautics, 1992. http://dx.doi.org/10.2514/6.1992-1302.

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9

Businger, Steven, Berrien Moore III, Carl A. Nardell, and Paul B. Hays. "GroundWinds Hawaii: Applications for wind profiles derived from an ultraviolet lidar in Hawaii." In International Symposium on Remote Sensing, edited by Ulrich Schreiber, Christian Werner, Gary W. Kamerman, and Upendra N. Singh. SPIE, 2002. http://dx.doi.org/10.1117/12.453991.

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10

McHugh, John. "Large Amplitude Waves Over Hawaii." In 47th AIAA Aerospace Sciences Meeting including The New Horizons Forum and Aerospace Exposition. Reston, Virigina: American Institute of Aeronautics and Astronautics, 2009. http://dx.doi.org/10.2514/6.2009-109.

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Звіти організацій з теми "Hawaiki"

1

Hudgens, Bian, Jene Michaud, Megan Ross, Pamela Scheffler, Anne Brasher, Megan Donahue, Alan Friedlander та ін. Natural resource condition assessment: Puʻuhonua o Hōnaunau National Historical Park. National Park Service, вересень 2022. http://dx.doi.org/10.36967/2293943.

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Natural Resource Condition Assessments (NRCAs) evaluate current conditions of natural resources and resource indicators in national park units (parks). NRCAs are meant to complement—not replace—traditional issue- and threat-based resource assessments. NRCAs employ a multi-disciplinary, hierarchical framework within which reference conditions for natural resource indicators are developed for comparison against current conditions. NRCAs do not set management targets for study indicators, and reference conditions are not necessarily ideal or target conditions. The goal of a NRCA is to deliver science-based information that will assist park managers in their efforts to describe and quantify a park’s desired resource conditions and management targets, and inform management practices related to natural resource stewardship. The resources and indicators emphasized in a given NRCA depend on the park’s resource setting, status of resource stewardship planning and science in identifying high-priority indicators, and availability of data and expertise to assess current conditions for a variety of potential study resources and indicators. Puʻuhonua o Hōnaunau National Historical Park (hereafter Puʻuhonua o Hōnaunau NHP) encompasses 1.7 km2 (0.7 mi2) at the base of the Mauna Loa Volcano on the Kona coast of the island of Hawaiʻi. The Kona coast of Hawaiʻi Island is characterized by calm winds that increase in the late morning to evening hours, especially in the summer when there is also a high frequency of late afternoon or early evening showers. The climate is mild, with mean high temperature of 26.2° C (79.2° F) and a mean low temperature of 16.6° C (61.9° F) and receiving on average 66 cm (26 in) of rainfall per year. The Kona coast is the only region in Hawaiʻi where more precipitation falls in the summer than in the winter. There is limited surface water runoff or stream development at Puʻuhonua o Hōnaunau NHP due to the relatively recent lava flows (less than 1,500 years old) overlaying much of the park. Kiʻilae Stream is the only watercourse within the park. Kiʻilae Stream is ephemeral, with occasional flows and a poorly characterized channel within the park. A stream gauge was located uphill from the park, but no measurements have been taken since 1982. Floods in Kiʻilae Stream do occur, resulting in transport of fluvial sediment to the ocean, but there are no data documenting this phenomenon. There are a small number of naturally occurring anchialine pools occupying cracks and small depressions in the lava flows, including the Royal Fishponds; an anchialine pool modified for the purpose of holding fish. Although the park’s legal boundaries end at the high tide mark, the sense of place, story, and visitor experience would be completely different without the marine waters adjacent to the park. Six resource elements were chosen for evaluation: air and night sky, water-related processes, terrestrial vegetation, vertebrates, anchialine pools, and marine resources. Resource conditions were determined through reviewing existing literature, meta-analysis, and where appropriate, analysis of unpublished short- and long-term datasets. However, in a number of cases, data were unavailable or insufficient to either establish a quantitative reference condition or conduct a formal statistical comparison of the status of a resource within the park to a quantitative reference condition. In those cases, data gaps are noted, and comparisons were made based on qualitative descriptions. Overall, the condition of natural resources within Puʻuhonua o Hōnaunau NHP reflects the surrounding landscape. The coastal lands immediately surrounding Puʻuhonua o Hōnaunau NHP are zoned for conservation, while adjacent lands away from the coast are agricultural. The condition of most natural resources at Puʻuhonua o Hōnaunau NHP reflect the overall condition of ecological communities on the west Hawai‘i coast. Although little of the park’s vegetation...
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Loose, Verne William, and Cesar Augusto Silva Monroy. Hawaii Electric System Reliability. Office of Scientific and Technical Information (OSTI), August 2012. http://dx.doi.org/10.2172/1113873.

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3

Metzger, I., and J. Salasovich. Hawaii-Okinawa Building Evaluations. Office of Scientific and Technical Information (OSTI), May 2013. http://dx.doi.org/10.2172/1083371.

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Silva Monroy, Cesar, and Verne Loose. Hawaii electric system reliability. Office of Scientific and Technical Information (OSTI), September 2012. http://dx.doi.org/10.2172/1090205.

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5

Rocheleau, Richard, Scott Turn, James Griffin, Arthur Maskrey, Michael Antal, Jr., Severine Busquet, Michael Cooney, et al. Hawaii Energy Sustainable Program. Office of Scientific and Technical Information (OSTI), December 2016. http://dx.doi.org/10.2172/1399265.

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6

Burgess, Lawrence. Hawaii Comprehensive Heart Program. Fort Belvoir, VA: Defense Technical Information Center, March 2010. http://dx.doi.org/10.21236/ada520734.

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7

Accius, Jean, and Suh Joo Yeoun. Longevity Economy Outlook Hawaii. Washington, DC: AARP Thought Leadership, September 2020. http://dx.doi.org/10.26419/int.00044.012.

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Burgess, Lawrence. Hawaii Comprehensive Heart Program. Fort Belvoir, VA: Defense Technical Information Center, March 2011. http://dx.doi.org/10.21236/ada549083.

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NAVAL OCEAN SYSTEMS CENTER SAN DIEGO CA. Base Exterior Architecture Plan: Naval Ocean Systems Center Hawaii Laboratory, Oahu, Hawaii. Fort Belvoir, VA: Defense Technical Information Center, February 1990. http://dx.doi.org/10.21236/ada222632.

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10

Sims, Jill. Hawaii Renewable Energy Development Venture. Office of Scientific and Technical Information (OSTI), October 2017. http://dx.doi.org/10.2172/1475063.

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