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RECORDS of the HAWAII BIOLOGICAL SURVEY for 1995 Part 2: Notes1
RECORDS OF THE HAWAII BIOLOGICAL SURVEY FOR 1995 Part 2: Notes1 This is the second of two parts to the Records of the Hawaii Biological Survey for 1995 and contains the notes on Hawaiian species of plants and animals including new state and island records, range extensions, and other information. Larger, more compre- hensive treatments and papers describing new taxa are treated in the first part of this Records [Bishop Museum Occasional Papers 45]. New Hawaiian Pest Plant Records for 1995 PATRICK CONANT (Hawaii Dept. of Agriculture, Plant Pest Control Branch, 1428 S King St, Honolulu, HI 96814) Fabaceae Ulex europaeus L. New island record On 6 October 1995, Hawaii Department of Land and Natural Resources, Division of Forestry and Wildlife employee C. Joao submitted an unusual plant he found while work- ing in the Molokai Forest Reserve. The plant was identified as U. europaeus and con- firmed by a Hawaii Department of Agriculture (HDOA) nox-A survey of the site on 9 October revealed an infestation of ca. 19 m2 at about 457 m elevation in the Kamiloa Distr., ca. 6.2 km above Kamehameha Highway. Distribution in Wagner et al. (1990, Manual of the flowering plants of Hawai‘i, p. 716) listed as Maui and Hawaii. Material examined: MOLOKAI: Molokai Forest Reserve, 4 Dec 1995, Guy Nagai s.n. (BISH). Melastomataceae Miconia calvescens DC. New island record, range extensions On 11 October, a student submitted a leaf specimen from the Wailua Houselots area on Kauai to PPC technician A. Bell, who had the specimen confirmed by David Lorence of the National Tropical Botanical Garden as being M. -
Can Hawaii Meet Its Renewable Fuel Target? Case Study of Banagrass-Based Cellulosic Ethanol
International Journal of Geo-Information Article Can Hawaii Meet Its Renewable Fuel Target? Case Study of Banagrass-Based Cellulosic Ethanol Chinh Tran * and John Yanagida Department of Natural Resources and Environmental Management, University of Hawaii at Manoa, 1910 East-West Road, Honolulu, HI 96822, USA; [email protected] * Correspondence: [email protected]; Tel.: +1-808-956-4065 Academic Editors: Shih-Lung Shaw, Qingquan Li, Yang Yue and Wolfgang Kainz Received: 9 March 2016; Accepted: 8 August 2016; Published: 16 August 2016 Abstract: Banagrass is a biomass crop candidate for ethanol production in the State of Hawaii. This study examines: (i) whether enough banagrass can be produced to meet Hawaii’s renewable fuel target of 20% highway fuel demand produced with renewable sources by 2020 and (ii) at what cost. This study proposes to locate suitable land areas for banagrass production and ethanol processing, focusing on the two largest islands in the state of Hawaii—Hawaii and Maui. The results suggest that the 20% target is not achievable by using all suitable land resources for banagrass production on both Hawaii and Maui. A total of about 74,224,160 gallons, accounting for 16.04% of the state’s highway fuel demand, can be potentially produced at a cost of $6.28/gallon. Lower ethanol cost is found when using a smaller production scale. The lowest cost of $3.31/gallon is found at a production processing capacity of about 9 million gallons per year (MGY), which meets about 2% of state demand. This cost is still higher than the average imported ethanol price of $3/gallon. -
Downloaded 10/07/21 11:20 PM UTC JULY 2010 C a R L I S E T a L
2706 MONTHLY WEATHER REVIEW VOLUME 138 Numerical Simulations of Island-Scale Airflow over Maui and the Maui Vortex under Summer Trade Wind Conditions DANA L. CARLIS* Howard University Program in Atmospheric Sciences, Washington, D.C., and Honolulu Weather Forecast Office, National Weather Service, Honolulu, Hawaii YI-LENG CHEN Department of Meteorology, University of Hawaii at Manoa, Honolulu, Hawaii VERNON R. MORRIS Howard University Program in Atmospheric Sciences, Howard University, Washington, D.C. (Manuscript received 22 September 2009, in final form 14 January 2010) ABSTRACT The fifth-generation Pennsylvania State University–NCAR Mesoscale Model (MM5) coupled with the Noah land surface model (LSM) is employed to simulate island-scale airflow and circulations over Maui County, Hawaii, under summer trade wind conditions, during July–August 2005. The model forecasts are validated by surface observations with good agreement. In this study, it is shown that a previously known closed circulation over the Central Valley of Maui, or the Maui vortex, represents the northern cyclonic vortex of the dual-counter-rotating vortices in the lee of Haleakala, which extend up to the base of the trade wind inversion with a westerly reversed flow (.2ms21). At low levels, the northern cyclonic vortex is more pronounced than the southern anticyclonic vortex. The asymmetric structure of the dual vortices is related to the shape of Haleakala and the flow deflection by the West Maui Mountains. The Maui vortex has a relatively narrow east–west extent in the lowest levels, espe- cially at night, due to the deflected strong northerly/northeasterly winds from the windward foothills of the West Maui Mountains. -
GRAND WAILEA FACT SHEET Situated on 40 Acres Fronting
GRAND WAILEA FACT SHEET Situated on 40 acres fronting spectacular Wailea Beach on the southwest shore of the island of Maui, the Grand Wailea is a 35-minute drive from the Kahului Airport and a 20-minute flight from Honolulu. Grand Wailea was built in 1991 with a commitment to portray the richness of Hawaii’s nature, culture and people. The resort features luxurious accommodations, award- winning cuisine, the unparalleled Spa Grande, championship golf and tennis, as well as the island’s most notable pools and water park. ACCOMMODATIONS The resort has 776 guestrooms, including 56 suites. The Napua Tower offers 100 rooms in a private club-area situated at the center of the hotel, featuring dedicated concierge services with upgraded guest room accommodations. Grand Wailea’s guest rooms are well designed and spacious, ranging from 640 square feet to 5,500 square feet. HO‛OLEI AT GRAND WAILEA The resort also offers luxury vacation villas with Ho‛olei at Grand Wailea - lavish private residences offering 3-bedroom, 3.5-bath luxury villas with the highest level of quality standards. Perfect for extended stays, special celebrations and family gatherings, Ho‛olei at Grand Wailea blends the finest in residential living, exceptional amenities and attentive services. Nestled in the center of the world-class Wailea Resort community and adjacent to Grand Wailea, the centerpiece of Ho‛olei at Grand Wailea is a lush tropical playground featuring a large pool with swim-in grotto and 19-foot waterfall, children's pool with a sandy beach entry and whirlpool tubs. Guests can enjoy a state-of-the-art fitness center with a private locker room complete with oversized showers and sauna. -
Island Studies Journal, Vol. 4, No. 2, 2009, Pp. 183-202 at The
Island Studies Journal , Vol. 4, No. 2, 2009, pp. 183-202 At the Intersection of Resident, Research and Recreation Stakeholder Interests: East Maui, Hawai‘i, as a Sustainable Tourism Destination John Cusick University of Hawai‘i at Manoa Oahu, Hawai‘i, USA [email protected] Abstract: The experiences of contemporary protected areas indicate adaptations to challenges brought about by resource management strategies. Resident communities, protected area management, and the tourism industry stakeholders demonstrate that evolving relationships are complex webs of competing and cooperating interests. The geographic isolation of East Maui delayed the cultural disruption of traditional practices and is an area where residents simultaneously resist assimilation and re-create cultural landscapes to offer visitors a glimpse into the past and a view of an emerging future associated with the renaissance of Native Hawaiian identity. Partnerships have brought about and nurtured the perpetuation of culture and the conservation of biodiversity as stakeholders recognize shared benefits. Among the outcomes are that residents have reconstituted the identity of East Maui as a Hawaiian place with benefits to various stakeholders, including a network of protected areas. A sustainability framework suggests a reappraisal of how to nurture, not alter, East Maui’s identity. Keywords : community based tourism, cultural kipuka, golf course development, Hana, Hawai‘i, islandness, Maui, protected areas, stakeholders, sustainability framework © 2009 – Institute of Island Studies, University of Prince Edward Island, Canada. Introduction The combination of biological diversity and cultural heritage is routinely cited as being conducive to the development of ecotourism activities (Honey, 1999; Stronza & Durham, 2008). An increase and expansion of tourism development associated with protected areas facilitate the convergence of stakeholder interests and raise issues related to resident place, research field site, and tourist destination (Howe et al ., 1997; Terborgh et al ., 2002). -
PDF Download Prevailing Trade Winds: Climate and Weather in Hawaii Kindle
PREVAILING TRADE WINDS: CLIMATE AND WEATHER IN HAWAII PDF, EPUB, EBOOK Marie Sanderson | 126 pages | 01 Feb 1994 | University of Hawai'i Press | 9780824814915 | English | Honolulu, HI, United States Prevailing Trade Winds: Climate and Weather in Hawaii PDF Book Usually by late morning, winds increase again due to the additional forcing effects from the sun. Annual weather conditions in Hawaii vary neigh. Still, we can look at the long-term trends and get a general idea of what to expect. Project Seasons of the Year on YouTube channel:. The persistent trades mean steady winds in summer months. These conditions are often accompanied by higher gusts above 40 kts. However, trends from one day to the next may be inferred. Received: 14 Feb Published Online: Oct This book is not yet featured on Listopia. The trade winds that continually blow across the island cause it to be permanently bent in one direction. Link Network. Community Reviews. Thanks for telling us about the problem. Past Climatic Changes Dennis Nullet. Currents are not well defined around the Hawaiian Islands. The best method to differentiate current direction and speed is visual observations of buoys and onboard instrumentation. The temperature falls about 3. Easterly Waves and Remnants of Tropical Cyclones: The most likely effect of tropical cyclones may come from the remains an earlier tropical cyclone or easterly wave. Cite Data - Experimental. Enjoy a CovidSafe visit to the National Library. Clouds on the leeward side often have localized cells that contain increased wind speed as a result of downdrafts. July 4 — Independence Day. Summer kau lasts from May through October, with high temperatures and reliable trade winds. -
West Honolulu Watershed Study
West Honolulu Watershed Study Final Report Prepared For: Honolulu Board of Water Supply Department of Land and Natural Resources, Engineering Division U.S. Army Corps of Engineers, Honolulu District Prepared By: Townscape, Inc. and Eugene P. Dashiell, AICP May 2003 West Honolulu Watershed Study - Final Report - Prepared for: HONOLULU BOARD OF WATER SUPPLY DEPARTMENT OF LAND AND NATURAL RESOURCES ENGINEERING DIVISION U.S. ARMY CORPS OF ENGINEERS HONOLULU DISTRICT Prepared by: Townscape, Inc. and Eugene P. Dashiell, AICP May 2003 This page intentionally left blank. West Honolulu Watershed Study FINAL REPORT WEST HONOLULU WATERSHED STUDY ACKOWLEDGEMENTS This study was conducted under the direction of the U.S. Army Corps of Engineers, Honolulu District (COE), through Section 22 of the Water Resources Development Act of 1974, as amended. Project manager for the West Honolulu Watershed Study was Derek Chow of COE, Engineer District, Honolulu. Local sponsorship for the study was provided jointly by the City and County of Honolulu Board of Water Supply, represented by Barry Usagawa, Principal Executive of the Water Resources Unit, and Scot Muraoka, Long-Range Planning Section; and the State of Hawaiÿi Department of Land and Natural Resources (DLNR), Engineering Division, which was represented by Sterling Yong, Head of the Flood Control and Dam Safety Section, and Eric Yuasa and Carty Chang of the Project Planning Section. The three co-sponsors of this study wish to acknowledge the following groups and individuals for their contribution to the West Honolulu Watershed Study: Principal Planner and President Bruce Tsuchida and Staff Planners Michael Donoho and Sherri Hiraoka of Townscape, Inc., contracted through the COE as the planning consultant for the study. -
The Rainfall Atlas of Hawai'i 2011
THE RAINFALL ATLAS OF HAWAI‘I 2011 Final Report Thomas W. Giambelluca1, Qi Chen1, Abby G. Frazier1, Jonathan P. Price2 Yi-Leng Chen3, Pao-Shin Chu3, and Jon K. Eischeid4 1Department of Geography, University of Hawai‘i at Mānoa, Honolulu, HI, USA 2Department of Geography and Environmental Sciences, University of Hawai‘i - Hilo, Hilo, HI, USA 3Department of Meteorology, University of Hawai‘i at Mānoa, Honolulu, HI, USA 4Cooperative Institute for Research in Environmental Science, University of Colorado, Boulder, CO, USA October 2011 The Rainfall Atlas of Hawai‘i 2011 Final Report Acknowledgments The 2011 Rainfall Atlas of Hawai‘i was developed under an agreement between the State of Hawai‘i Commission on Water Resource Management and the U.S. Army Corps of Engineers, Honolulu District under Section 22 of the Water Resources Development Act of 1974. Contract No. W9128A-04-D-0019, Contract Task Order No. 0038 was awarded to Wil Chee Planning, Inc., which subcontracted the work to the University of Hawai‘i at Mānoa, Department of Geography. The development of the 2011 Rainfall Atlas of Hawai‘i was supported by numerous individuals and organizations. Please see the “People” tab of the Rainfall Atlas of Hawai‘i web site (http://rainfall.geography.hawaii.edu) for information about those who contributed to this work. We are grateful to the people listed there, as well as the many other individuals who contributed to Hawai‘i’s rainfall dataset by carefully and consistently making measurements and recording and preserving the data. Those records are an invaluable resource, without which no rainfall map analysis would be possible. -
Hilo Talk 9-2017
Outline The big picture - what controls the climate of Hawaii? Do our volcanos control on the climate of Hawaii Island? Changes to summit climate since mid last century The cloud forest and cloud layer changes Think global act local Mauna Kea Climate, Past and Future by Steven Businger, Professor and Chair Department of Atmospheric Sciences, UHM 1 2 3 4 Fall Equinox Friday was the autumnal equinox, so called because day and night have equal length. Also, interestingly, the border between day and night, called the terminator, is oriented exactly north-south, as seen in the visible satellite image at right. • The Earth’s spectral signature (color) is a product of our planet’s teeming life. Oxygen, which we breathe, and ozone, that shields us from UV radiation, are the products of photosythesis, and scatter blue light. Earth’s vegetation reflects red light. The resulting U-shaped spectrum, if seen in other planets, can help us to identify habitable planets. 5 6 Bird Bird Exodus Exodus Weather radar even tells us Our feathered friends know the which direction the birds are season is turning, with a massive flying. Here is the Doppler southward migration going on. How Velocity at 7:54 PM HST last do I know. Weather radar! Thurs, using the Camano Here is the radar image from 8:03 Island radar. It tells you the HST last Thursday night. Lots of component of motion echo..but no rain. Those are birds. towards or away from the How can I be sure? There was no radar. Cold colors (like blue) echo before sunset and then the indicate incoming, warm radar lit up as it got dark. -
Preliminary Environmental Assessment for MAUI ELECTRIC COMPANY REQUEST for PROPOSALS for VARIABLE RENEWABLE DISPATCHABLE GENERATION
Preliminary Environmental Assessment FOR MAUI ELECTRIC COMPANY REQUEST FOR PROPOSALS FOR VARIABLE RENEWABLE DISPATCHABLE GENERATION KAHANA SOLAR PROJECT MAUI, HAWAII Prepared for: Innergex Renewables USA, LLC 1185 West George Street, Suite 900 Vancouver, British Columbia V6E 4E6 Prepared by: Tetra Tech, Inc. 737 Bishop Street, Suite 2340 Honolulu, HI 96813 November 2019 PRELIMINARY EA FOR MECO RFP RESPONSE Table of Contents Introduction ............................................................................................................................................................... 1 1.1 Project Description .................................................................................................................................. 1 Natural Environment ............................................................................................................................................. 3 2.1 Air Quality ................................................................................................................................................... 3 2.1.1 Existing conditions .................................................................................................................. 3 2.1.2 Short- and Long-Term Impacts .......................................................................................... 3 2.1.3 Best Management Practices and Mitigation .................................................................. 4 2.2 Biology ......................................................................................................................................................... -
Thirty-Four Years of Hawaii Wave Hindcast from Downscaling of Climate Forecast System Reanalysis
1 Ocean Modelling Achimer April 2016, Volume 100 Pages 78-95 http://dx.doi.org/10.1016/j.ocemod.2016.02.001 http://archimer.ifremer.fr http://archimer.ifremer.fr/doc/00313/42425/ © 2016 Elsevier Ltd. All rights reserved. Thirty-four years of Hawaii wave hindcast from downscaling of climate forecast system reanalysis Li Ning 1, Cheung Kwok Fai 1, *, Stopa Justin 2, Hsiao Feng 3, Chen Yi-Leng 3, Vega Luis 4, Cross Patrick 4 1 Department of Ocean and Resources Engineering, University of Hawaii, Honolulu, HI 96822, USA 2 Laboratoire d’Oceanographie Spatiale, Ifremer, Plouzane, France 3 Department of Atmospheric Sciences, University of Hawaii, Honolulu, HI 96822, USA 4 Hawaii Natural Energy Institute, University of Hawaii, Honolulu, HI 96822, USA * Corresponding author : Cheung Kwok Fai, Tel.: +1 808 956 3485 ; fax: +1 808 956 3498 ; Email address : [email protected] [email protected] ; [email protected] ; [email protected] ; [email protected] ; [email protected] ; [email protected] Abstract : The complex wave climate of Hawaii includes a mix of seasonal swells and wind waves from all directions across the Pacific. Numerical hindcasting from surface winds provides essential space-time information to complement buoy and satellite observations for studies of the marine environment. We utilize WAVEWATCH III and SWAN (Simulating WAves Nearshore) in a nested grid system to model basin-wide processes as well as high-resolution wave conditions around the Hawaiian Islands from 1979 to 2013. The wind forcing includes the Climate Forecast System Reanalysis (CFSR) for the globe and downscaled regional winds from the Weather Research and Forecasting (WRF) model. -
SECTION 4. RISK ASSESSMENT 4.15Wildfire
State of Hawaiʻi 2018 | Hazard Mitigation Plan SECTION 4. RISK ASSESSMENT 4.15Wildfire 2018 HMP UPDATE CHANGES The hazard profile has been significantly enhanced to include a detailed hazard description, location, extent, previous occurrences, and probability of future occurrence (including how climate change may impact the hazard). New and updated figures from federal and state agencies are incorporated. Wildfire events that occurred in the State of Hawai‘i from January 1, 2012 through December 31, 2017 were researched for this 2018 HMP Update. The high wildfire risk areas provided by the Hawai‘i Wildfire Management Organization were used to assess vulnerability (HWMO 2013). 4.15.1 Hazard Profile Wildfires in the State of Hawai‘i destroy native forests, alter soil composition, and threaten human safety and infrastructure. The State of Hawaii’s native ecosystems are not fire adapted. In many cases, once an area burns, it is replaced by fire-prone non-native species, permanently changing the State of Hawaii’s landscape. Over 25% of the State contains non-native, fire-prone grasses and shrubs which fuels the fires that occur in the State. This percentage grows each time fire burns into native forest because the forest is then further invaded by fire prone non-native species (Hawai‘i Wildfire Management Organization [HWMO] 2016a). Each year, approximately 0.5% of the State of Hawaii’s total land area burns, which is equal to or greater than the proportion burned of any other state. Over 98% of the total wildfires are human-caused. In the last 10 years, nearly 1,000 wildfires burned an average of 20,000 acres per year statewide.