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  • 1
    Publication Date: 2021-08-05
    Description: We analyze how winter thaw events (TE; T〉0°C) are changing on the summit of Mount Washington, New Hampshire using three metrics: the number of TE, number of thaw hours, and number of thaw degree-hours for temperature and dewpoint for winters from 1935-36 to 2019-20. The impact of temperature-only-TE and dewpoint-TE on snow depth are compared to quantify the different impacts of sensible-only and sensible-and-latent heating, respectively. Results reveal that temperature- and dewpoint-TE for all metrics increased at a statistically significant rate (p
    Print ISSN: 1558-8424
    Electronic ISSN: 1558-8432
    Topics: Geography , Physics
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  • 2
    Publication Date: 2022-06-06
    Description: Author Posting. © American Meteorological Society, 2021. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Applied Meteorology and Climatology 60(9), (2021): 1361–1370, https://doi.org/10.1175/JAMC-D-20-0254.1.
    Description: We analyze how winter thaw events (TE; T 〉 0°C) are changing on the summit of Mount Washington, New Hampshire, using three metrics: the number of TE, number of thaw hours, and number of thaw degree-hours for temperature and dewpoint for winters from 1935/36 to 2019/20. The impact of temperature-only TE and dewpoint TE on snow depth are compared to quantify the different impacts of sensible-only heating and sensible-and-latent heating, respectively. Results reveal that temperature and dewpoint TE for all metrics increased at a statistically significant rate (p 〈 0.05) over the full time periods studied for temperature (1935/36–2019/20) and dewpoint (1939/40–2019/20). Notably, around 2000/01, the positive trends increased for most variables, including dewpoint-thaw degree-hours that increased by 82.11 degree-hours decade−1 during 2000–20, which is approximately 5 times as faster as the 1939–2020 rate of 17.70 degree-hours decade−1. Furthermore, a clear upward shift occurred around 1990 in the lowest winter values of thaw hours and thaw degree-hours—winters now have a higher baseline amount of thaw than before 1990. Snow-depth loss during dewpoint TE (0.36 cm h−1) occurred more than 2 times as fast as temperature-only TE (0.14 cm h−1). With winters projected to warm throughout the twenty-first century in the northeastern United States, it is expected that the trends in winter thaw events, and the sensible and latent energy that they bring, will continue to rise and lead to more frequent winter flooding, fewer days of good quality snow for winter recreation, and changes in ecosystem function.
    Keywords: Atmosphere ; Snowmelt/icemelt ; Snowpack ; Winter/cool season ; Climate change ; Humidity ; Latent heating/cooling ; Snow cover ; Temperature
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 3
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-06-01
    Description: This data was collected by a team led by Kirincich as part of a Metocean monitoring campaign sponsored by the Massachusetts Clean Energy Center (MassCEC). The campaign was designed to observe key atmospheric and ocean parameters at an existing offshore platform in the proximity of the Massachusetts and Rhode Island Wind Energy Areas. The campaign supported the purchase and installation of a LIDAR wind profiler, two cup anemometers and a wind direction vane at the MVCO Air-Sea Interaction Tower (ASIT). These instruments were installed and operated by WHOI and validated by UL-AWS Truepower following a MetOcean Measurement Plan created by UL-AWST, WHOI, and the MassCEC. All instruments were installed on WHOI's offshore tower in the fall of 2016 and operated continuously, as possible, through the end of 2020. After this time the project transitioned to become the MetOcean Reference Site (MORS-1), supported by the National Offshore Wind Research and Development Consortium (NOWRDC).
    Repository Name: Woods Hole Open Access Server
    Type: Other
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  • 4
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-06-01
    Description: This zipped content contains Lidar summary data: Daily 10-minute average files from 53-200m amsl for 2021.
    Repository Name: Woods Hole Open Access Server
    Type: Dataset
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  • 5
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-06-01
    Description: Meteorological tower daily data for 2021
    Repository Name: Woods Hole Open Access Server
    Type: Dataset
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  • 6
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-06-01
    Description: Meteorological tower monthly summary data for 2021
    Repository Name: Woods Hole Open Access Server
    Type: Dataset
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  • 7
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-06-01
    Description: This report compares the wind characteristics of Lidar WLS7 436, a Windcube v2.0 lidar, and Lidar ZX1166, a ZX Lidars ZX300M, comprising part of the Met Ocean Reference Station (MORS-1) situated on the Air-Sea Interaction Tower (ASIT) located approximately 3 km south of Martha’s Vineyard in 17-m of water. The ASIT is a cabled, fixed platform that has a maximum height of 23 m above mean sea level (MSL) and a platform located at 13 m MSL. The ASIT operates within the Martha’s Vineyard Coastal Observatory (MVCO) facility established in 2001 and is operated by Woods Hole Oceanographic Institution (WHOI). Remote sensing data collection commenced at the ASIT in October 2016 with the initial deployment of Lidar WLS7 436 as part of a metocean initiative funded by the Massachusetts Clean Energy Center (MassCEC)1. WHOI later established the MORS-1 campaign in 2021. Lidar ZX1166, a calibrated ZX Lidars ZX300M, was deployed to the ASIT platform on 1 September 2021. Lidar WLS7 436 was removed from the platform on 8 October 2021. Site information, a table of concurrent mean wind speeds at each measurement level between 60 m and 200 m, scatterplots of concurrent wind speeds at each measurement level between 60 m and 200 m, wind speed frequency distributions and wind roses at two key measurement levels, and a plot of concurrent wind shear are presented below for the period that the two lidars were present on the ASIT platform. For their concurrent period of record, wind speed and direction data at the same measurement levels agreed closely between the two lidars.
    Repository Name: Woods Hole Open Access Server
    Type: Other
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  • 8
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-06-01
    Description: On behalf of Woods Hole Oceanographic Institution (“WHOI”), UL Services Group LLC (“UL”) conducted a verification1 of a ground-based remote sensing device (“RSD”) according to IEC 61400-12-1 Ed. 2 [1] Annex L. The Lidar ZX 300M was collocated with a 130 m mast at UL’s Advanced Wind Turbine Test Facility at West Texas A&M University, near Canyon, Texas. This report describes the measurement site, the mast and RSD equipment, and the results from the verification. The verification results include the linear regression relationships between wind speed, wind direction, shear, and turbulence intensity for each coincident height.
    Repository Name: Woods Hole Open Access Server
    Type: Other
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  • 9
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-06-01
    Description: Unit is located on an Ocean met mast. There is a platform approximately 11 meter off the water line. with another 15 meters of lattice tower above it. The site is approximately 2.75 kilometers off the Southeast coast of Martha’s Vineyard.
    Repository Name: Woods Hole Open Access Server
    Type: Other
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  • 10
    Publication Date: 2022-12-01
    Description: This data was collected by Kirincich as part of the NSF-sponsored High Frequency Radar Winds program, with the goal of understanding the errors in present day HFR-based wind extraction algorithms that are due to variations in the signal losses along the transmission path. Understanding variations in the received power levels for land-based high frequency radar systems is critical to advancing radar-based estimates of winds and waves. We use a long-term record of one-way high frequency radar power observations to explore the key factors controlling propagation losses over the ocean. Observed propagation loss was quantified using an 8-month record of radio frequency (RF) power from a shore-based transmitter, received at two locations: an offshore tower and a nearby island. Observations were compared to environmental factors as well as models of path loss incorporating smooth and rough surface impedances and varying atmospheric properties. Significant differences in the observations at the two sites existed. One-way path loss variations at the tower, a wavelength above mean sea level, were closely related to atmospheric forcing, while variations at the distant island site were dominated by wind-driven surface gravity wave variability. Seasonal variability in ocean conductivity had no significant effect on over-ocean path losses. Simplistic analytical models of path loss were found to have more skill than either ground wave propagation models or more complex numerical models of field strength in matching the observations, due in part to under-observation of the atmosphere but also the differences in rough surface impedance between models of ocean waves.
    Description: Funded by NSF Award # OCE-1923927 and NSF Award # OCE-1923465.
    Keywords: High frequency Radar ; Path loss ; Martha’s Vineyard ; Martha’s Vineyard Coastal Observatory ; Nantucket ; Surface atmospheric observations ; Surface ocean observations
    Repository Name: Woods Hole Open Access Server
    Type: Dataset
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