The Red Edge Problem in asteroid band parameter analysis

Meteoritics and Planetary Science Wiley 51:4 (2016) 806-817

Authors:

Sean S Lindsay, Tasha L Dunn, Joshua P Emery, Neil E Bowles

Inflight Radiometric Calibration of New Horizons' Multispectral Visible Imaging Camera (MVIC)

(2016)

Authors:

CJA Howett, AH Parker, CB Olkin, DC Reuter, K Ennico, WM Grundy, AL Graps, KP Harrison, HB Throop, MW Buie, JR Lovering, SB Porter, HA Weaver, LA Young, SA Stern, RA Beyer, RP Binzell, BJ Buratti, AF Cheng, JC Cook, DP Cruikshank, CM Dalle Ore, AM Earle, DE Jennings, IR Linscott, AW Lunsford, J Wm Parker, S Phillippe, S Protopapa, E Quirico, PM Schenk, B Schmitt, KN Singer, JR Spencer, JA Stansberry, CCC Tsang, GE Weigle, AJ Verbiscer

New temperature and pressure retrieval algorithm for high-resolution infrared solar occultation spectroscopy: analysis and validation against ACE-FTS and COSMIC

Atmospheric Measurement Techniques Copernicus Publications 9:3 (2016) 1063-1082

Authors:

Kevin S Olsen, Geoffrey C Toon, Chris D Boone, Kimberly Strong

Global energy budgets and 'Trenberth diagrams' for the climates of terrestrial and gas giant planets

Quarterly Journal of the Royal Meteorological Society Wiley 142:695 (2016) 703-720

Authors:

Peter L Read, Joanna Barstow, Benjamin Charnay, Sivapalan Chelvaniththilan, Patrick GJ Irwin, Sylvia Knight, Sebastien Lebonnois, Stephen R Lewis, Joao Mendonça, Luca Montabone

Abstract:

The climate on Earth is generally determined by the amount and distribution of incoming solar radiation, which must be balanced in equilibrium by the emission of thermal radiation from the surface and atmosphere. The precise routes by which incoming energy is transferred from the surface and within the atmosphere and back out to space, however, are important features that characterize the current climate. This has been analysed in the past by several groups over the years,based on combinations of numerical model simulations and direct observations of theEarths climate system. The results are often presented in schematic form to show the main routes for the transfer of energy into, out of and within the climate system. Although relatively simple in concept, such diagrams convey a great deal of information about the climate system in a compact form. Such an approach has not so far been widely adopted in any systematic way for other planets of the Solar System, let alone beyond, although quite detailed climate models of several planets are now available, constrained bymany new observations and measurements. Here we present an analysis of the global transfers of energy within the climate systems of a range of planets within the Solar System,including Mars, Titan, Venus a nd Jupit er, a s mo delled by rela t ively co mprehens iveradiative transfer and (in some cases) numerical circulation models. These results are presented in schematic form for comparison with the classical global energy budget analyses (e.g.Trenberth et al. 2009; Stephenset al.2012; Wildet al.2013; IPCC 2013)for the Earth, highlighting important similarities and differences. We also take the first steps towards extending this approach to other Solar System and extra-solar planets,including Mars, Venus, Titan, Jupiter and the ‘hot Jupiter’ exoplanet HD189733b, presenting a synthesis of `both previously published and new calculations for all of these planets.

How to decarbonize? Look to Sweden

Bulletin of the Atomic Scientists Routledge 72:2 (2016) 105-111

Abstract:

Bringing global warming to a halt requires that worldwide net emissions of carbon dioxide be brought to essentially zero, and the sooner this occurs, the less warming our descendants for the next thousand years and more will need to adapt to. The widespread fear that the actions needed to bring this about conflict with economic growth is a major impediment to efforts to protect the climate. However, much of this fear is pointless, and the magnitude of the task, while great, is no greater than challenges human ingenuity has surmounted in the past. To light the way forward, there is a need for examining success stories in which nations have greatly reduced their carbon dioxide emissions while simultaneously maintaining vigorous growth in the standard of living. In this article, the example of Sweden is showcased. Through a combination of sensible government infrastructure policies and free-market incentives, Sweden has managed to successfully decarbonize, cutting its per capita emissions by a factor of three since the 1970s, while doubling its pre capita income and providing a wide range of social benefits. This has all be accomplished within a vigorous capitalistic framework which in many ways embodies freemarket principles better than the economy of the United States.