Reflecting Sunlight to Cool Earth
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Marine Cloud Brightening
MARINE CLOUD BRIGHTENING Alan Gadian , John Latham, Mirek Andrejczuk, Keith Bower, Tom Choularton, Hugh Coe, Paul Connolly, Ben Parkes, Phillip Rasch, Stephen Salter, Hailong Wang and Rob Wood . Contents:- • Background to the philosophical approach • Some L.E.M . and climate model results • Technological issues. • Future plans and publications. Science Objectives:- • To explain the science of how stratocumulus clouds can have a significant effect on the earth’s radiation balance • To present some modelling results from Latham et al 2011 Marine Cloud Brightening, WRCP October 2011 1 Stratocumulus clouds cover more than 30% of ocean surface Stratocumulus clouds have a high reflectance, which depends on droplet number and mean droplet size. Twomey Effect .:- Smaller drops produce whiter clouds . Proposal :- To advertently to enhance the droplet concentration N in low-level maritime stratocumulus clouds, so increasing cloud albedo (Twomey, JAS, 1977 ) and longevity ( Albrecht, Science, 1989 ) Technique:- To disseminate sea-water droplets of diameter about 1um at the ocean surface. Some of these ascend via turbulence to cloud-base where they are activated to form cloud droplets, thereby enhancing cloud droplet number concentration, N (Latham, Nature 1990 ; Phil Trans Roy Soc 2008 and 2011, under review ) 2 Above:- Computed spherical albedo for increasing pollution in THIN, MEDIUM and THICK clouds. ( Twomey, JAS, 1977 ) Right:- Frequency distributions of the reflectances at 1,535 nm versus reflectances at 754 nm. From ACE-2. Isolines of geometrical thickness (H) and droplet number concentration (N): higher reflectance in polluted cloud, normalised by a similar geometrical thickness (Brenguier et al. 2000 ). 3 Figure 1. Panel (a): Map of MODIS-derived annual mean cloud droplet concentration N 0 for stratiform marine warm clouds. -
Climate Change, Consequentialism, and the Road Ahead
Chicago Journal of International Law Volume 13 Number 2 Article 8 1-1-2013 Climate Change, Consequentialism, and the Road Ahead Dale Jamieson Follow this and additional works at: https://chicagounbound.uchicago.edu/cjil Recommended Citation Jamieson, Dale (2013) "Climate Change, Consequentialism, and the Road Ahead," Chicago Journal of International Law: Vol. 13: No. 2, Article 8. Available at: https://chicagounbound.uchicago.edu/cjil/vol13/iss2/8 This Article is brought to you for free and open access by Chicago Unbound. It has been accepted for inclusion in Chicago Journal of International Law by an authorized editor of Chicago Unbound. For more information, please contact [email protected]. Climate Change, Consequentialism, and the Road Ahead Dale Jamieson* Abstract In this paperI tell the stoy of the evolution of the climate change regime, locating its origins in "the dream of Rio," which supposed that the nations of the world would join in addressing the interlocking crises of environment and development. I describe the failure at Copenhagen and then go on to discuss the "reboot" of the climate negoiations advocated by Eric A. Posner and David Weisbach. I bring out some ambiguides in their notion of InternationalPareianism, which is supposed to effectively limit the influence of moral ideals in internationalaffairs, and pose a dilemma. I go on to discuss the foundations of their views regarding climate justice, arguing that the most reasonable understandings of their favored theoretical views would not lead to some of their conclusions. Finaly, I return to the climate regime, and make some observations about the road ahead, concluding thatfor theforeseeable future the most important climate change action will be within countries rather than among them. -
1 Equitably Ending the Fossil Fuel Era: Climate Justice, Capital, & The
Equitably Ending the Fossil Fuel Era: Climate Justice, Capital, & the Carbon Budget Georges Alexandre Lenferna A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy University of Washington 2019 Reading Committee: Stephen Gardiner, Chair Carina Fourie Aseem Prakash Michael Blake Program Authorized to Offer Degree: Department of Philosophy 1 ©Copyright 2019 Georges Alexandre Lenferna 2 University of Washington Abstract Equitably Ending the Fossil Fuel Era: Climate Justice, Capital, & the Carbon Budget Georges Alexandre Lenferna Chair of the Supervisory Committee: Stephen Gardiner Department of Philosophy This dissertation makes the moral case for equitably transitioning away from fossil fuels in line with keeping global warming as close as possible to the Paris Climate Agreement’s more stringent target of keeping global warming to 1.5°C above pre-industrial levels. It argues that we should do so while relying as little as possible on risky and uncertain negative emissions and geoengineering technologies, as doing so might prolong the fossil fuel era and pose grave potential costs both to the present and future generations. The dissertation addresses a central objection to the moral imperative to transition away from fossil fuels, namely that it will detrimentally impact the poor and vulnerable. It argues in response that protecting the interests of the poor and vulnerable is best achieved through a rapid yet just transition away from fossil fuels. Based on the moral case to transition away from fossil fuels in line with 1.5°C the dissertation also explores what personal moral responsibility individuals have to take action to reduce fossil fuel usage and act on climate change. -
CLIMATE RISK COUNTRY PROFILE: GHANA Ii ACKNOWLEDGEMENTS This Profile Is Part of a Series of Climate Risk Country Profiles Developed by the World Bank Group (WBG)
CLIMATE RISK COUNTRY PROFILE GHANA COPYRIGHT © 2021 by the World Bank Group 1818 H Street NW, Washington, DC 20433 Telephone: 202-473-1000; Internet: www.worldbank.org This work is a product of the staff of the World Bank Group (WBG) and with external contributions. The opinions, findings, interpretations, and conclusions expressed in this work are those of the authors and do not necessarily reflect the views or the official policy or position of the WBG, its Board of Executive Directors, or the governments it represents. The WBG does not guarantee the accuracy of the data included in this work and do not make any warranty, express or implied, nor assume any liability or responsibility for any consequence of their use. This publication follows the WBG’s practice in references to member designations, borders, and maps. The boundaries, colors, denominations, and other information shown on any map in this work, or the use of the term “country” do not imply any judgment on the part of the WBG, its Boards, or the governments it represents, concerning the legal status of any territory or geographic area or the endorsement or acceptance of such boundaries. The mention of any specific companies or products of manufacturers does not imply that they are endorsed or recommended by the WBG in preference to others of a similar nature that are not mentioned. RIGHTS AND PERMISSIONS The material in this work is subject to copyright. Because the WBG encourages dissemination of its knowledge, this work may be reproduced, in whole or in part, for noncommercial purposes as long as full attribution to this work is given. -
Exploring the MBL Cloud and Drizzle Microphysics Retrievals from Satellite, Surface and Aircraft
Exploring the MBL cloud and drizzle microphysics retrievals from satellite, surface and aircraft Xiquan Dong, University of Arizona Pat Minnis, SSAI 1. Briefly describe our 2. Can we utilize these surface newly developed retrieval retrievals to develop cloud (and/or drizzle) Re profile for algorithm using ARM radar- CERES team? lidar, and comparison with aircraft data. Re is a critical for radiation Wu et al. (2020), JGR and aerosol-cloud- precipitation interactions, as well as warm rain process. 1 A long-term Issue: CERES Re is too large, especially under drizzling MBL clouds A/C obs in N Atlantic • Cloud droplet size retrievals generally too high low clouds • Especially large for Re(1.6, 2.1 µm) CERES Re too large Worse for larger Re • Cloud heterogeneity plays a role, but drizzle may also be a factor - Can we understand the impact of drizzle on these NIR retrievals and their differences with Painemal et al. 2020 ground truth? A/C obs in thin Pacific Sc with drizzle CERES LWP high, tau low, due to large Re Which will lead to high SW transmission at the In thin drizzlers, Re is overestimated by 3 µm surface and less albedo at TOA Wood et al. JAS 2018 Painemal et al. JGR 2017 2 Profiles of MBL Cloud and Drizzle Microphysical Properties retrieved from Ground-based Observations and Validated by Aircraft data during ACE-ENA IOP 푫풎풂풙 ퟔ Radar reflectivity: 풁 = ퟎ 푫 푵풅푫 Challenge is to simultaneously retrieve both cloud and drizzle properties within an MBL cloud layer using radar-lidar observations because radar reflectivity depends on the sixth power of the particle size and can be highly weighted by a few large drizzle drops in a drizzling cloud 3 Wu et al. -
FOIA) Document Clearinghouse in the World
This document is made available through the declassification efforts and research of John Greenewald, Jr., creator of: The Black Vault The Black Vault is the largest online Freedom of Information Act (FOIA) document clearinghouse in the world. The research efforts here are responsible for the declassification of hundreds of thousands of pages released by the U.S. Government & Military. Discover the Truth at: http://www.theblackvault.com Received Received Request ID Requester Name Organization Closed Date Final Disposition Request Description Mode Date 17-F-0001 Greenewald, John The Black Vault PAL 10/3/2016 11/4/2016 Granted/Denied in Part I respectfully request a copy of records, electronic or otherwise, of all contracts past and present, that the DOD / OSD / JS has had with the British PR firm Bell Pottinger. Bell Pottinger Private (legally BPP Communications Ltd.; informally Bell Pottinger) is a British multinational public relations and marketing company headquartered in London, United Kingdom. 17-F-0002 Palma, Bethania - PAL 10/3/2016 11/4/2016 Other Reasons - No Records Contracts with Bell Pottinger for information operations and psychological operations. (Date Range for Record Search: From 01/01/2007 To 12/31/2011) 17-F-0003 Greenewald, John The Black Vault Mail 10/3/2016 1/13/2017 Other Reasons - Not a proper FOIA I respectfully request a copy of the Intellipedia category index page for the following category: request for some other reason Nuclear Weapons Glossary 17-F-0004 Jackson, Brian - Mail 10/3/2016 - - I request a copy of any available documents related to Army Intelligence's participation in an FBI counterintelligence source operation beginning in about 1959, per David Wise book, "Cassidy's Run," under the following code names: ZYRKSEEZ SHOCKER I am also interested in obtaining Army Intelligence documents authorizing, as well as policy documents guiding, the use of an Army source in an FBI operation. -
Climate Litigation and Atmospheric Ethics: a Case Study of Juliana V
CLIMATE LITIGATION AND ATMOSPHERIC ETHICS: A CASE STUDY OF JULIANA V. UNITED STATES Mark Ortiz A thesis submitted to the faculty at the University of North Carolina at Chapel Hill in partial fulfillment of the requirements for the degree of Master of Arts in the Department of Geography. Chapel Hill 2017 Approved By: Elizabeth Olson Elizabeth Havice Scott Kirsch ©2017 Mark Ortiz ALL RIGHTS RESERVED ii ABSTRACT Mark Ortiz: Climate Litigation and Atmospheric Ethics: A Case Study of Juliana v. United States (Under the Direction of: Drs. Elizabeth Olson and Elizabeth Havice) This thesis offers an account of climate change lawsuits as ethical experiments which endeavor to develop legal and ethical norms and principles suited to a world remolded by cumulative human actions. It offers a theorization of the ‘what’ and the ‘why’ of the growing, global wave of climate litigation by situating it within the dynamic landscape of contemporary climate politics. Through a case study of Juliana v. United States, a first-of-its-kind constitutional climate lawsuit against the United States federal government, this thesis examines how legal narrative is mobilized to give ethical shape and significance to the problem of climate change and to conceptualize responsibility across vast sweeps of space and time. Interweaving insights from climate ethics, environmental humanities, legal geography and science and technology studies, this research offers a set of meditations on atmospheric ethics iii TABLE OF CONTENTS CHAPTER 1: INTRODUCTION: CLIMATE LITIGATION AS ETHICAL EXPERIMENTATION ................................................................................................. 1 1.1 Introduction ................................................................................................................... 1 1.2 Methods, Approach and Plan of the Present Work ....................................................... 5 1.3 Climate Ethics: Sculpting the Climatic Citizen ........................................................... -
7.2 DEVELOPMENT of a METEOROLOGICAL PARTICLE SENSOR for the OBSERVATION of DRIZZLE Richard Lewis* National Weather Service St
7.2 DEVELOPMENT OF A METEOROLOGICAL PARTICLE SENSOR FOR THE OBSERVATION OF DRIZZLE Richard Lewis* National Weather Service Sterling, VA 20166 Stacy G. White Science Applications International Corporation Sterling, VA 20166 1. INTRODUCTION “Very small, numerous, and uniformly dispersed, water drops that may appear to float while The National Weather Service (NWS) and Federal following air currents. Unlike fog droplets, drizzle Aviation Administration (FAA) are jointly participating in a falls to the ground. It usually falls from low Product Improvement Program to improve the capabilities stratus clouds and is frequently accompanied by of the of Automated Surface Observing Systems (ASOS). low visibility and fog. The greatest challenge in the ASOS was to automate the visual elements of the observation; sky conditions, visibility In weather observations, drizzle is classified as and type of weather. Despite achieving some success in (a) “very light”, comprised of scattered drops that this area, limitations in the reporting capabilities of the do not completely wet an exposed surface, ASOS remain. As currently configured, the ASOS uses a regardless of duration; (b) “light,” the rate of fall Precipitation Identifier that can only identify two being from a trace to 0.25 mm per hour: (c) precipitation types, rain and snow. A goal of the Product “moderate,” the rate of fall being 0.25-0.50 mm Improvement program is to replace the current PI sensor per hour:(d) “heavy” the rate of fall being more with one that can identify additional precipitation types of than 0.5 mm per hour. When the precipitation importance to aviation. Highest priority is being given to equals or exceeds 1mm per hour, all or part of implementing capabilities of identifying ice pellets and the precipitation is usually rain; however, true drizzle. -
ESSENTIALS of METEOROLOGY (7Th Ed.) GLOSSARY
ESSENTIALS OF METEOROLOGY (7th ed.) GLOSSARY Chapter 1 Aerosols Tiny suspended solid particles (dust, smoke, etc.) or liquid droplets that enter the atmosphere from either natural or human (anthropogenic) sources, such as the burning of fossil fuels. Sulfur-containing fossil fuels, such as coal, produce sulfate aerosols. Air density The ratio of the mass of a substance to the volume occupied by it. Air density is usually expressed as g/cm3 or kg/m3. Also See Density. Air pressure The pressure exerted by the mass of air above a given point, usually expressed in millibars (mb), inches of (atmospheric mercury (Hg) or in hectopascals (hPa). pressure) Atmosphere The envelope of gases that surround a planet and are held to it by the planet's gravitational attraction. The earth's atmosphere is mainly nitrogen and oxygen. Carbon dioxide (CO2) A colorless, odorless gas whose concentration is about 0.039 percent (390 ppm) in a volume of air near sea level. It is a selective absorber of infrared radiation and, consequently, it is important in the earth's atmospheric greenhouse effect. Solid CO2 is called dry ice. Climate The accumulation of daily and seasonal weather events over a long period of time. Front The transition zone between two distinct air masses. Hurricane A tropical cyclone having winds in excess of 64 knots (74 mi/hr). Ionosphere An electrified region of the upper atmosphere where fairly large concentrations of ions and free electrons exist. Lapse rate The rate at which an atmospheric variable (usually temperature) decreases with height. (See Environmental lapse rate.) Mesosphere The atmospheric layer between the stratosphere and the thermosphere. -
Exercise 10: Cumulus Cloud with Bulk Cloud Physics
Exercise Hints Tasks Results Exercise 10: Cumulus Cloud With Bulk Cloud Physics PALM group Institute of Meteorology and Climatology, Leibniz Universität Hannover last update: 21st September 2015 PALM group PALM Seminar 1 / 16 I Initialize the simulation with a marine, cumulus-topped, trade-wind region boundary layer. I Trigger the cloud by a bubble of rising warm air. I Parameterize condensation using a simple bulk cloud physics scheme. I Learn how to carry out conditional averages. Exercise Hints Tasks Results Exercise Exercise 10: Cumulus Cloud With Bulk Cloud Physics Simulate a cumulus cloud: PALM group PALM Seminar 2 / 16 I Trigger the cloud by a bubble of rising warm air. I Parameterize condensation using a simple bulk cloud physics scheme. I Learn how to carry out conditional averages. Exercise Hints Tasks Results Exercise Exercise 10: Cumulus Cloud With Bulk Cloud Physics Simulate a cumulus cloud: I Initialize the simulation with a marine, cumulus-topped, trade-wind region boundary layer. PALM group PALM Seminar 2 / 16 I Parameterize condensation using a simple bulk cloud physics scheme. I Learn how to carry out conditional averages. Exercise Hints Tasks Results Exercise Exercise 10: Cumulus Cloud With Bulk Cloud Physics Simulate a cumulus cloud: I Initialize the simulation with a marine, cumulus-topped, trade-wind region boundary layer. I Trigger the cloud by a bubble of rising warm air. PALM group PALM Seminar 2 / 16 I Learn how to carry out conditional averages. Exercise Hints Tasks Results Exercise Exercise 10: Cumulus Cloud With Bulk Cloud Physics Simulate a cumulus cloud: I Initialize the simulation with a marine, cumulus-topped, trade-wind region boundary layer. -
Climate Change Guidelines for Forest Managers for Forest Managers
0.62cm spine for 124 pg on 90g ecological paper ISSN 0258-6150 FAO 172 FORESTRY 172 PAPER FAO FORESTRY PAPER 172 Climate change guidelines Climate change guidelines for forest managers for forest managers The effects of climate change and climate variability on forest ecosystems are evident around the world and Climate change guidelines for forest managers further impacts are unavoidable, at least in the short to medium term. Addressing the challenges posed by climate change will require adjustments to forest policies, management plans and practices. These guidelines have been prepared to assist forest managers to better assess and respond to climate change challenges and opportunities at the forest management unit level. The actions they propose are relevant to all kinds of forest managers – such as individual forest owners, private forest enterprises, public-sector agencies, indigenous groups and community forest organizations. They are applicable in all forest types and regions and for all management objectives. Forest managers will find guidance on the issues they should consider in assessing climate change vulnerability, risk and mitigation options, and a set of actions they can undertake to help adapt to and mitigate climate change. Forest managers will also find advice on the additional monitoring and evaluation they may need to undertake in their forests in the face of climate change. This document complements a set of guidelines prepared by FAO in 2010 to support policy-makers in integrating climate change concerns into new or -
Exam 2: Cloud Physics April 16, 2008 Physical Meteorology 3440
Name ____________________________ Exam 2: Cloud Physics April 16, 2008 Physical Meteorology 3440 Questions 1-10 are worth 5 points each. Questions 11-15 are worth 10 points each. 1. Rank the concentrations of the following from lowest (1) to highest (3): cloud condensation nuclei (3) cloud droplets (2) raindrops (1) 2. Match the following particles with their typical size cloud condensation nuclei 10 μm cloud droplets 0.1 μm raindrops 1000 μm 3. Why do ice crystals grow at the expense of supercooled water droplets? The saturation vapor pressure over liquid is higher than the saturation vapor pressure over ice. Therefore, the environment will be more supersaturated with respect to ice than with respect to liquid, and the ice crystals will grow more quickly. At some point, the ice crystals may bring S (with respect to ice) down to 1, in which case Sl (with respect to liquid) is less than 1, causing the liquid drops to evaporate. 4. Match the following particles with their most likely means of growth 5 μm cloud drop accretion 5 μm ice crystal aggregation 100 μm dendritic ice crystals in ice cloud depositional growth 500 μm ice crystal in mixed-phase cloud condensational growth 100 μm cloud drop collision-coalescence 5. Fill in the blanks: Not all clouds with temperatures below the freezing point of water contain ice, because of the scarcity of ice nuclei in the atmosphere, and the temperature at which they nucleate ice. As the cloud temperature decreases, the probability of ice increases to the 1 temperature of -40 °C, at which point homogeneous freezing occurs.