Inn-I-Isen-Opplevelse Paul A. Dodd Norsk Polarinstitutt, Tromsø NP-Dagen – 14 Mars 2014.

Slides:



Advertisements
Similar presentations
Coupled Arctic Regional Atmosphere-Ocean-Sea Ice Model Minwei Qian and Colin Jones.
Advertisements

What? Remote, actively researched, monitored, measured, has a huge impact on global climate and is relatively cool?
Physical Oceanography
The syllabus says: Atmosphere and change  Describe the functioning of the atmospheric system in terms of the energy balance between solar and long- wave.
A thermodynamic model for estimating sea and lake ice thickness with optical satellite data Student presentation for GGS656 Sanmei Li April 17, 2012.
CliC (NEG) Climate and Cryosphere Recent, current and planned activities Aike Beckmann
Collaborative Research on Sunlight and the Arctic Atmosphere-Ice-Ocean System (AIOS) Hajo Eicken Univ. of Alaska Fairbanks Ron Lindsay Univ. of Washington.
Collaborative Investigation of Climate Cryosphere Interaction 3 (CICCI 3) Rune Storvold, Norut/NTNU NySMAC, Helsinki, April 7 th -8 th, 2014.
UNIVERSITY OF LEEDS School of Earth and Environment INSTITUTE FOR CLIMATE AND ATMOSPHERIC SCIENCE Arctic Summer Cloud-Ocean Study (ASCOS) Ian Brooks, Cathryn.
1.Sea Ice and Snow cover -Evidences As they melt mountain glaciers leave behind the an altered landscape with low albedo. a. shrinking glacial are around.
Climatic changes in the last 200 years (Ch. 17 & 18) 1. Is it warming? --climate proxy info (recap) -- info from historical & instrumental records 2. What.
Disko Bay, Greenland - 624,000 cubic miles of ice; 10% of Earth’s fresh water.
Parameters and instruments A. Proshutinsky, Woods Hole Oceanographic Institution Science and Education Opportunities for an Arctic Cabled Seafloor Observatory.
By the early 18th Century nearly every residence had a cesspit beneath the floors. In the best of homes the nauseating stench permeated the most elegant.
Climate science in a world with global change David Noone Program in Atmospheric and Oceanic Sciences Cooperative Institute for Research in Environmental.
Foundation Sea Surface Temperature W. Emery, S. Castro and N. Hoffman From Wikipedia: Sea surface temperature (SST) is the water temperature close to the.
Overview of the Past and Present Earth System Observations of the Earth OSHR 1609 Climate 101 September 20, 2013 Scott Denning, CSU.
Challenges in Modeling Global Sea Ice in a Changing Environment Marika M Holland National Center for Atmospheric Research Marika M Holland National Center.
Dr. Wara Simon Teoh Daniel leong. Arctic ice cap is in trouble sea ice cover has been disappearing at approximately 70,000 km 2 per year ice has grown.
Surface air temperature. Review of last lecture Earth’s energy balance at the top of the atmosphere and at the surface. What percentage of solar energy.
4. Models of the climate system. Earth’s Climate System Sun IceOceanLand Sub-surface Earth Atmosphere Climate model components.
Chapter 13- Polar and highland climates temperature is key (again) cold due to limited solar radiation low angle of incidence of insolation Moisture is.
US CLIVAR Themes. Guided by a set of questions that will be addressed/assessed as a concluding theme action by US CLIVAR Concern a broad topical area.
Sea Ice. Big Questions: What are the quantitative contributions of various processes to ice mass balance over the annual cycle. What positive and negative.
The Future of Arctic Sea Ice Authors: Wieslaw Maslowski, Jaclyn Clement Kinney, Matthew Higgins, and Andrew Roberts Brian Rosa – Atmospheric Sciences.
LIVE INTERACTIVE YOUR DESKTOP Thursday, March 25, 2010 Presented by: Dr. Lisa Gardiner An Introduction to Earth’s Climate.
Charge to the Working Group How well do we understand the 2007 sea ice extent minimum? (through modelling and data analysis including retrospective analyses.
The Atmosphere. Did you know we are on our 3 atmosphere on Earth? Earth’s original atmosphere was probably just hydrogen and helium, because these were.
The polar sea ice covers are large Tens of millions of square kilometers, and empty.
Outline Further Reading: Detailed Notes Posted on Class Web Sites Natural Environments: The Atmosphere GE 101 – Spring 2007 Boston University Myneni L30:
The U.S. Inter-agency Arctic Research Policy Committee (IARPC) 5-year Research Plan, FY13-FY17 1.Understand sea-ice dynamics, ecosystem processes, ecosystem.
6.4.8: Explain how convection affects weather patterns and climate.
Dr. Frank Herr Ocean Battlespace Sensing S&T Department Head Dr. Scott L. Harper Program Officer Team Lead, 322AGP Dr. Martin O. Jeffries Program Officer.
Global warming and Sea Level Rise: Best estimates by 2100 John King
NACLIM CT1/CT3 1 st CT workshop April 2013 Hamburg (DE) Johann Jungclaus.
This section of the documentary focused on the Oceans and how Global Climate Change will affect them.
Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial.
Global Climate Change. 150 Authors 1,000 Contributing Authors 5 Years Work 130 Countries 1,000 Expert Reviewers The IPCC WGI Report.
S 1 Core Theme 1 Predictability of core ocean and atmosphere quantities UHAM, MPG, UPMC, GEOMAR, NERSC.
LIVE INTERACTIVE YOUR DESKTOP May 17, 2011 NASA Earth Climate Course Presented by: Marge Marcy.
The Atmosphere: Energy Transfer & Properties Weather Unit Science 10.
Antarctic Sea Ice and Polynyas
© Crown copyright Met Office The Role of Research Aircraft in YOPP Chawn Harlow, YOPP Summit, WMO, Geneva 13 July 2015.
Land cover & fire at high latitudes: model-data comparison and model modification NCEO Land Science Meeting, February 2012, Sheffield, UK E.Kantzas,
Weather and Climate Vocabulary 3-5 Grade. Rain Gauge An Instrument Used To Measure The Amount of Rainfall.
Preliminary modeling work simulating N-ICE snow distributions and the associated impacts on: 1)sea ice growth; 2)the formation of melt ponds; and 3)the.
AIM: How the “spheres” interact: The Water Cycle
AOMIP status Experiments 1. Season Cycle 2. Coordinated - Spinup Coordinated - Analysis Coordinated 100-Year Run.
Multidisciplinary drifting Observatory for the Study of Arctic Climate
The Multidisciplinary drifting Observatory
Snow measurements during N_ICE JC Gallet 1, G. Liston 2 and S. Gerland 1 1 Norwegian Polar Institute, Tromsø, Norway 2 Colorado State University 17 November.
Weather and Climate Vocabulary 3-5 Grade. Rain Gauge An instrument used to measure the amount of rainfall.
Describes the condition of the atmosphere such as temperature, cloud cover, wind speed, and rainfall.
ENERGY AND THE WATER CYCLE (NASA Animation) 2 AIM: HOW THE “SPHERES” INTERACT: THE WATER CYCLE.
Metrics and MODIS Diane Wickland December, Biology/Biogeochemistry/Ecosystems/Carbon Science Questions: How are global ecosystems changing? (Question.
An advanced snow parameterization for the models of atmospheric circulation Ekaterina E. Machul’skaya¹, Vasily N. Lykosov ¹Hydrometeorological Centre of.
HOW GLOBAL WARMING HAS AFFECTED GLACIERS By: Tunyasiri & Kankanit P.3.
How Convection Currents Affect Weather and Climate.
MOSAiC Meeting, ASSW, 13 March 2016, Fairbanks Townhall Meeting 13 March :00 – 17:00 Multidisciplinary drifting Observatory for the Study of Arctic.
Lecture 10: Ice on Earth EarthsClimate_Web_Chapter.pdfEarthsClimate_Web_Chapter.pdf, p. 8, 27-30; Ch. 2, p. 21; Ch. 10, p I.Sea Ice II.Glacial.
Chapter 4: Weather and Climate Notes
Climate Change Climate – The average year after year pattern of temperature, precipitation, winds and clouds in an area. Climates are classified mainly.
Exam review: study guide
Radiation Balance and Feedbacks
Natural Causes of Climate Change
Electromagnetic Radiation
WORLD CLIMATE RESEARCH PROGRAMME
Exam review: study guide
Climate Change – Causes and Impacts
Presentation transcript:

Inn-I-Isen-Opplevelse Paul A. Dodd Norsk Polarinstitutt, Tromsø NP-Dagen – 14 Mars 2014

Where Do We Plan To Go?

Start ~15 Jan 2015 near N 83º 15’, E030º 00’ Probably out drift out through Fram Strait by late April 2015 Re-freeze near again near N 83º 15’, E030º 00’ Drift until to 1st week of July, 2015 Helicopter flights approximately every 21 days to change scientists & crew.

Preparing Lance for the N-ICE 2015: DECK:  New shelter for CTD & multinet  Winch for multinet  Extended range of sonar for multinet  Container labs  Freezer container  Heating mats  Heating cables in water intake.  Telescopic Crane to replace existing two cranes LABS: Filtered seawater Filtered freshwater Fume-cupboard for chemicals Chemical storage cupboards Lots of attachment points for equiptment

What Are We Trying to Find Out? Primary objective: To understand the effects of the new thin, first year, sea ice regime in the Arctic on energy flux, ice dynamics and the ice associated ecosystem, and local and global climate. Secondary objectives: Understand how available ocean heat is mixed upwards towards the sea ice and to what extent it influences the sea ice energy budget. Understand the fate of solar radiation incident on the first-year sea ice in the region and how its fate is affected by properties of the atmosphere, snow, ice, and ocean. Quantification of the changing mass balance of Arctic sea ice and its snow cover. Model the dynamics of the drifting ice. Understand the ice associated ecosystem and model future changes. Effects on local and global weather systems.

WP1: Upper Ocean – Sea Ice Interaction Understand how available ocean heat is mixed upwards, towards the sea ice, and to what extent it influences the sea-ice energy budget.

WP2: Atmospheric Forcing Understand and quantify atmospheric processes driving snow and ice growth and melt, upper ocean heating, including the role of clouds, and some mass fluxes between ice-ocean-atmosphere such as CO 2

Quantify the changing mass balance of Arctic sea ice and its snow cover, with consideration of feedback processes affecting the speed of changes, for assessing the relevance of mass balance changes for the treatment of sea ice in climate models WP3: Sea Ice and Snow Mass Balance

WP4: Sea Ice Dynamics High precision, continuous observations of regional scale sea-ice drift and deformation to evaluate and improve satellite-derived drift datasets and model simulations.

WP5: Biogeochemical Sea Ice Interactions Understand links between physical mechanisms and biogeochemical processes, emphasizing their reciprocal feedbacks in the Marginal Ice.

Overview of Measurement Sites:

The N-ICEtest cruise (21 February – 03 March 2014) Penetrated to 82º 30’ N, 030º 00’ E To test instruments and modifications to Lance Practise working in the cold and dark Moored to the ice for 4 days and set up instruments Evacuation during the night of 26th February, due to wave action Evacuation Time-lapse Video

Thank you for listening! The trip home: 50 knot wind 8m waves 0 scientists standing up… Photo: Alexey Pavlov