Bolometric Hemispherical Albedo Map of Pluto from New Horizons Observations Data Set Overview ================= The NASA New Horizons encounter with the Pluto system in 2015 revealed Pluto to have an extraordinary range of surface albedos, abundant volatile and refractory ices, and complex geology from endogenous and exogenous processes (Stern et al., 2015). Pluto is an active world with ongoing convective and glacial resurfacing, seasonal volatile transport that includes nitrogen and methane cycles, and chemical processing by ionizing radiation (e.g., Gladstone et al., 2016; Grundy et al., 2016; Moore et al., 2016). Photometric properties of a surface, including albedo, are useful for constraining volatile transport by quantifying absorbed solar energy, as well as for providing insights into surface processes. For example, albedo measurements can contribute to relative estimates of processing, mixing, temporal variability, and age for different terrains. This dataset is a map of Pluto's incidence-angle-average bolometric hemispherical albedo. Hemispherical albedo is the ratio of total power scattered by a surface, where total refers to integration over all emission angles, to incident power. Bolometric hemispherical albedo is the flux-weighted, wavelength-integrated ratio and is crucial for understanding the thermal behavior of a surface. The map was produced using the best-fit lunar-Lambert photometric functions for Pluto's extreme dark and bright terrains, Cthulhu and Sputnik Planitia (some names are informal), as representative of low and high reflectance regions and by approximating intermediate reflectance regions as a linear combination of these two extremes. New Horizons Long Range Reconnaissance Imager (LORRI) panchromatic and Multispectral Visible Imaging Camera (MVIC) panchromatic, blue, and red filter observations were used to approximate bolometric albedo. The LORRI and MVIC data were from the NASA Planetary Data System (PDS) Small Bodies Node (SBN) v3.0 archive. Regions south of 38 degrees South were in winter darkness (polar night) during the New Horizons flyby of Pluto and the map does not include areas south of approximately 30 degrees South. The map was produced using the USGS Integrated Software for Imagers and Spectrometers (ISIS). The mapping group parameters are: ProjectionName = Equirectangular CenterLongitude = 180.0 CenterLatitude = 0.0 TargetName = pluto EquatorialRadius = 1188300 PolarRadius = 1188300 LatitudeType = Planetocentric LongitudeDirection = PositiveEast LongitudeDomain = 360 MinimumLatitude = -49.381884697957 MaximumLatitude = 90.0 MinimumLongitude = 0.0 MaximumLongitude = 360.0 PixelResolution = 879.23076275961 Pluto's incidence-angle-average bolometric hemispherical albedo, spatially-averaged over areas north of approximately 30 degrees South, is approximately 0.54. Pluto has three general albedo categories: 1) very low albedo southern equatorial terrains including Cthulhu, 2) high albedo terrains that constitute most of Pluto’s surface, and 3) very high albedo terrains including Sputnik Planitia. Pluto’s extraordinary albedo variability with location is also spatially sharp at some places. Users are strongly encouraged to read the publication titled 'Bolometric Hemispherical Albedo Map of Pluto from New Horizons Observations' in the Planetary Science Journal by Hofgartner et al. in 2023 for further information, including data used, methods, uncertainty, and interpretation. We thank the entire NASA New Horizons team for enabling the production of this map. Financial support from the NASA New Frontiers Data Analysis Program (NFDAP) is gratefully acknowledged (Grant Number 80NSSC22K1118). Constructive reviews of the map and documentation by Jian-Yang Li, Xiao-Duan Zou, and the SBN team improved this archive.