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PSD-10CloudandAerosolProcesses<br />

FEDERAL LEADS: TANEIL UTTAL AND TIM SCHNEIDER<br />

CIRES LEAD: MATTHEW SHUPE<br />

NOAA Goal 2: Climate<br />

Project Goal: Make observations of clouds, aerosols and<br />

water vapor over a variety of ice, land and sea surfaces us<strong>in</strong>g<br />

a multi-sensor, multi-plat<strong>for</strong>m approach to improve retrieval<br />

techniques useful <strong>for</strong> satellite validation studies.<br />

Milestone 1. Produce cloud macrophysical and microphysical<br />

data sets describ<strong>in</strong>g the clouds at Arctic atmospheric<br />

observatories. These data sets will <strong>in</strong>clude <strong>in</strong><strong>for</strong>mation on<br />

cloud occurrence, vertical distribution, boundaries, phase<br />

and microphysical properties.<br />

There has been ongo<strong>in</strong>g work to develop and evaluate<br />

techniques <strong>for</strong> deriv<strong>in</strong>g cloud macrophysical, microphysical<br />

and dynamical properties from remote sensor measurements<br />

<strong>in</strong> order to produce cont<strong>in</strong>uous data sets from<br />

ongo<strong>in</strong>g Arctic observatory measurements and periodic<br />

observational campaigns. Many of these data sets are made<br />

available via public data archives supported by NOAA<br />

and other agencies. Dur<strong>in</strong>g the past year, two papers were<br />

published document<strong>in</strong>g some of these cloud data sets. The<br />

first paper documented cloud fraction measurements from<br />

long-term measurements (at least approximately one year<br />

<strong>in</strong> duration) from six Arctic atmospheric observatories,<br />

<strong>in</strong>clud<strong>in</strong>g a characterization of cloud boundaries, vertical<br />

distribution and persistence. The second paper looked <strong>in</strong><br />

more detail at cloud phase occurrence at three of the observatories<br />

with more complete and complex <strong>in</strong>strument suites.<br />

These studies revealed important differences <strong>in</strong> the annual<br />

distribution and occurrence of clouds at different Arctic<br />

locations, which could be l<strong>in</strong>ked to processes that control<br />

cloud phase and ultimately to the larger-scale meteorological<br />

environment at these locations. Additionally, a new set<br />

of comprehensive cloud measurements has been started<br />

at Summit, Greenland, and will eventually lead to further<br />

cloud properties data sets.<br />

Product: Shupe, MD, VP Walden, E Eloranta, T Uttal, JR<br />

Campbell, SM Starkweather, and M Shiobara (<strong>2011</strong>), Clouds<br />

at Arctic Atmospheric Observatories, Part I: Occurrence and<br />

macrophysical properties, J. Appl. Meteor. Clim., 50, 626-644.<br />

Shupe, MD (<strong>2011</strong>), Clouds at Arctic Atmospheric Observatories,<br />

Part II: Thermodynamic phase characteristics,<br />

J. Appl. Meteor. Clim., 50, 645-661.<br />

Milestone 2: Utilize ground-based, multi-<strong>in</strong>strument,<br />

remote-sensor measurements, aircraft <strong>in</strong> situ observations<br />

and high-resolution mesoscale models to study the role of<br />

cloud dynamical-microphysical processes <strong>in</strong> the Arctic cloud<br />

life cycle. Specific observations will come from various sites,<br />

<strong>in</strong>clud<strong>in</strong>g NOAA’s Study of Arctic <strong>Environmental</strong> Change,<br />

SEARCH; the DOE’s ARM sites, and the Surface Heat Budget<br />

of the Arctic, SHEBA; Arctic Summer Cloud Ocean Study,<br />

ASCOS; and Arctic Mechanisms of Interaction between the<br />

Surface and Atmosphere, AMISA, field campaigns.<br />

Coord<strong>in</strong>ated observational and model<strong>in</strong>g ef<strong>for</strong>ts have<br />

substantially enhanced our understand<strong>in</strong>g of cloud microphysical<br />

and dynamical processes that are responsible <strong>for</strong><br />

the persistence of Arctic strati<strong>for</strong>m clouds. Observationally,<br />

ef<strong>for</strong>ts have focused on deriv<strong>in</strong>g detailed <strong>in</strong><strong>for</strong>mation on<br />

<strong>in</strong>-cloud dynamical and microphysical properties and determ<strong>in</strong><strong>in</strong>g<br />

how these <strong>in</strong>teract both with<strong>in</strong> the cloud and the<br />

102 CIRES Annual Report <strong>2011</strong><br />

surround<strong>in</strong>g atmosphere. These observational analyses have<br />

led to a number of papers (<strong>in</strong> preparation or published)<br />

that document the observed cloud and boundary layer<br />

structure and suggest some ways <strong>in</strong> which aerosol properties<br />

constra<strong>in</strong> the <strong>for</strong>mation of ice particles <strong>in</strong> mixed-phase<br />

clouds. The detailed observational data have also been used<br />

to evaluate nested Weather <strong>Research</strong> and Forecast<strong>in</strong>g (WRF)<br />

model simulations, where the <strong>in</strong>nermost nest is run at very<br />

f<strong>in</strong>e scale resolutions of 50 meters or less. These high-resolution<br />

simulations, with proper large scale <strong>for</strong>c<strong>in</strong>g, are able<br />

to well capture the evolution of a strati<strong>for</strong>m, mixed-phase<br />

cloud system, lend<strong>in</strong>g confidence <strong>in</strong> many of the <strong>in</strong>ternal<br />

model processes. The model has then been used to exam<strong>in</strong>e<br />

moisture and energy budgets with<strong>in</strong> the cloud and atmosphere<br />

that cannot be directly observed. Thus, the model<br />

simulations have been a key tool <strong>for</strong> extend<strong>in</strong>g our understand<strong>in</strong>g<br />

of processes like entra<strong>in</strong>ment and mix<strong>in</strong>g beyond<br />

observational capabilities. Much of this general understand<strong>in</strong>g<br />

has been synthesized <strong>in</strong> a collaborative review article on<br />

persistent Arctic mixed-phase clouds that is currently under<br />

review.<br />

Product: De Boer, G, H Morrison, MD Shupe, and R Hildner<br />

(<strong>2011</strong>), Evidence of liquid dependent ice nucleation <strong>in</strong><br />

high-latitude strati<strong>for</strong>m clouds from surface remote sensors,<br />

Geophys. Res. Lett., 38, L01803, doi:10.1029/2010GL046016.<br />

Lance, S, MD Shupe, G Fe<strong>in</strong>gold, CA Brock, J Cozic, JS<br />

Holloway, RH Moore, A Nenes, JP Schwarz, JR Spackman,<br />

KD Froyd, DM Murphy, J Brioude, OR Cooper, A Stohl, and<br />

JF Burkhart (<strong>2011</strong>), CCN as a modulator of ice processes <strong>in</strong><br />

Arctic mixed-phase clouds, Atmos. Chem. Phys. Discuss., 11,<br />

6737-6770.<br />

Solomon, A, MD Shupe, POG Persson, and H Morrison<br />

(<strong>2011</strong>), Moisture and dynamical <strong>in</strong>teractions ma<strong>in</strong>ta<strong>in</strong><strong>in</strong>g<br />

decoupled Arctic mixed-phase stratocumulus <strong>in</strong> the presence<br />

of a humidity <strong>in</strong>version, Atmos. Chem. Phys. Discuss., 11,<br />

13469-13524.<br />

Morrison, H, G de Boer, G Fe<strong>in</strong>gold, J Harr<strong>in</strong>gton, MD<br />

Shupe, and K Sulia (<strong>2011</strong>), Self-organization and resilience of<br />

Arctic mixed-phase clouds, Nat. Geosci., submitted.<br />

Milestone 3. Participate <strong>in</strong> the Northwest Tropical Atlantic<br />

Salmon, NTAS; PIRATA Northeast Extension, PNE;<br />

and CalNex research cruises <strong>in</strong> 2010. Deploy cloud radar,<br />

radiometer and flux systems to measure key surface mar<strong>in</strong>e<br />

boundary layer parameters, low cloud macrophysical,<br />

microphysical and radiative properties. Conduct <strong>in</strong>itial<br />

analysis focused on the associations between low clouds<br />

and the boundary layer structure.<br />

The CIRES-NOAA team participated <strong>in</strong> the PIRATA (Prediction<br />

and <strong>Research</strong> Moored Array <strong>in</strong> the Tropical Atlantic)<br />

Northeast Extension (PNE; also referred to as Aerose) cruise<br />

<strong>in</strong> May 2010. Data have been made available via the NOAA<br />

Earth System <strong>Research</strong> Laboratory/Physical <strong>Sciences</strong> Division<br />

data archive and ftp site. Analysis of the data has been<br />

delayed.<br />

PSD-11 WaterCycle<br />

FEDERAL LEAD: MARTY RALPH<br />

CIRES LEAD: DAVID KINGSMILL<br />

NOAA Goal 3: Weather and Water<br />

Project Goal: Improve weather and climate predictions

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