Wave runup on a 1 on 10 slope /

Bibliography: p. 25.

The slope of lake surfaces under variable wind stresses /

Mode of access: Internet.

A report on the general soil areas and slope classes in small watersheds, Broome County, New York / by Carl S. Pearson.

Two folded maps in pocket.

High Uintas South Slope land management plan and final environmental statement /

Cover title.

The performance of the null-reference glide-slope system in presence of deep snow, 1975-1976 /

Mode of access: Internet.

Streaks of squatter of life, and far-west scenes ; a series of humorous sketches descriptive of incidents and characters in the wild West ; to which are added other miscellaneous pieces /

Also published with title: Western scenes ; or, Life on the prairie.

Alternatives workbook for the south slope development concept plan : Denali National Park and Preserve, Alaska.

Mode of access: Internet.

The Pacific slope and Alaska /

Mode of access: Internet.

Conservation farming in the Slope-Hettinger Soil Conservation District, North Dakota /

"June 1950"--Cover.

Streaks of life,

Recollections of the Empress Eugénie.--A fresh start and two portraits.--Two glimplses of Queen Victoria.--'Mount Music.'--An adventure in a train.--The quotation-fiend.--A winter of storm.--The opera fiasco.--An open secret.

High-resolution dynamical downscaling products for the North Slope of Alaska and surrounding areas, links to model result files

Climatic changes are most pronounced in northern high latitude regions. Yet, there is a paucity of observational data, both spatially and temporally, such that regional-scale dynamics are not fully captured, limiting our ability to make reliable projections. In this study, a group of dynamical downscaling products were created for the period 1950 to 2100 to better understand climate change and its impacts on hydrology, permafrost, and ecosystems at a resolution suitable for northern Alaska. An ERA-interim reanalysis dataset and the Community Earth System Model (CESM) served as the forcing mechanisms in this dynamical downscaling framework, and the Weather Research & Forecast (WRF) model, embedded with an optimization for the Arctic (Polar WRF), served as the Regional Climate Model (RCM). This downscaled output consists of multiple climatic variables (precipitation, temperature, wind speed, dew point temperature, and surface air pressure) for a 10 km grid spacing at three-hour intervals. The modeling products were evaluated and calibrated using a bias-correction approach. The ERA-interim forced WRF (ERA-WRF) produced reasonable climatic variables as a result, yielding a more closely correlated temperature field than precipitation field when long-term monthly climatology was compared with its forcing and observational data. A linear scaling method then further corrected the bias, based on ERA-interim monthly climatology, and bias-corrected ERA-WRF fields were applied as a reference for calibration of both the historical and the projected CESM forced WRF (CESM-WRF) products. Biases, such as, a cold temperature bias during summer and a warm temperature bias during winter as well as a wet bias for annual precipitation that CESM holds over northern Alaska persisted in CESM-WRF runs. The linear scaling of CESM-WRF eventually produced high-resolution downscaling products for the Alaskan North Slope for hydrological and ecological research, together with the calibrated ERA-WRF run, and its capability extends far beyond that. Other climatic research has been proposed, including exploration of historical and projected climatic extreme events and their possible connections to low-frequency sea-atmospheric oscillations, as well as near-surface permafrost degradation and ice regime shifts of lakes. These dynamically downscaled, bias corrected climatic datasets provide improved spatial and temporal resolution data necessary for ongoing modeling efforts in northern Alaska focused on reconstructing and projecting hydrologic changes, ecosystem processes and responses, and permafrost thermal regimes. The dynamical downscaling methods presented in this study can also be used to create more suitable model input datasets for other sub-regions of the Arctic.