Is a Concordat over Ukraine now conceivable with Mishka the bear? CEPS Commentary, 21 December 2014

With the tumultuous year of ever-changing episodes in Ukraine coming to a close – from Yanukovich reneging at Vilnius last November, to the new Maidan, to Yanukovich fleeing for his life, to Russia’s annexation of Crimea and incursions into the eastern Donbass, the election of pro-European President Poroshenko, the war with over 4,000 dead, the election of a new pro-European parliament and now the crash of the rouble – Michael Emerson sees at last a possible the end-game in sight. In this commentary, he sketches the essential elements of a Concordat to be struck between Russia, Ukraine and the West that would allow the eastern Donbass to be drawn into more normal processes of political and economic negotiation and the badly wounded Russia to gradually return to more normal international relations.

Seasonal mean air temperatures and ice phenology characteristics of Great Bear Lake and Great Slave Lake (2002-2009)

Time series of brightness temperatures (T(B)) from the Advanced Microwave Scanning Radiometer-Earth Observing System (AMSR-E) are examined to determine ice phenology variables on the two largest lakes of northern Canada: Great Bear Lake (GBL) and Great Slave Lake (GSL). T(B) measurements from the 18.7, 23.8, 36.5, and 89.0 GHz channels (H- and V- polarization) are compared to assess their potential for detecting freeze-onset/melt-onset and ice-on/ice-off dates on both lakes. The 18.7 GHz (H-pol) channel is found to be the most suitable for estimating these ice dates as well as the duration of the ice cover and ice-free seasons. A new algorithm is proposed using this channel and applied to map all ice phenology variables on GBL and GSL over seven ice seasons (2002-2009). Analysis of the spatio-temporal patterns of each variable at the pixel level reveals that: (1) both freeze-onset and ice-on dates occur on average about one week earlier on GBL than on GSL (Day of Year (DY) 318 and 333 for GBL; DY 328 and 343 for GSL); (2) the freeze-up process or freeze duration (freeze-onset to ice-on) takes a slightly longer amount of time on GBL than on GSL (about 1 week on average); (3) melt-onset and ice-off dates occur on average one week and approximately four weeks later, respectively, on GBL (DY 143 and 183 for GBL; DY 135 and 157 for GSL); (4) the break-up process or melt duration (melt-onset to ice-off) lasts on average about three weeks longer on GBL; and (5) ice cover duration estimated from each individual pixel is on average about three weeks longer on GBL compared to its more southern counterpart, GSL. A comparison of dates for several ice phenology variables derived from other satellite remote sensing products (e.g. NOAA Interactive Multisensor Snow and Ice Mapping System (IMS), QuikSCAT, and Canadian Ice Service Database) show that, despite its relatively coarse spatial resolution, AMSR-E 18.7 GHz provides a viable means for monitoring of ice phenology on large northern lakes.

Point clouds of measurements in the Dechen Cave near Iserlohn, Germany

Modeling natural phenomena from 3D information enhances our understanding of the environment. Dense 3D point clouds are increasingly used as highly detailed input datasets. In addition to the capturing techniques of point clouds with LiDAR, low-cost sensors have been released in the last few years providing access to new research fields and facilitating 3D data acquisition for a broader range of applications. This letter presents an analysis of different speleothem features using 3D point clouds acquired with the gaming device Microsoft® Kinect. We compare the Kinect sensor with terrestrial LiDAR reference measurements using the KinFu pipeline for capturing complete 3D objects (< 4m**3). The results demonstrate the suitability of the Kinect to capture flowstone walls and to derive morphometric parameters of cave features. Although the chosen capturing strategy (KinFu) reveals a high correlation (R2=0.92) of stalagmite morphometry along the vertical object axis, a systematic overestimation (22% for radii and 44% for volume) is found. The comparison of flowstone wall datasets predominantly shows low differences (mean of 1 mm with 7 mm standard deviation) of the order of the Kinect depth precision. For both objects the major differences occur at strongly varying and curved surface structures (e.g. with fine concave parts).

Particulate concentrations and vertical fluxes of sedimentary material and chemical elements, composition of particulate and sinking material in the water column of the Bear Island Trough, Norwegian Sea, July 1995

CTD and nephelometric sounding data are considered along with parameters of the near-bottom currents and particulate fluxes measured by a subsurface mooring station in the northern part of the Bear Island Trough. It is shown that the near-bottom current is characterized by highly variable parameters, while distribution of suspended particulate matter demonstrates surface and bottom maxima. Horizontal and vertical fluxes of sedimentary material in the nepheloid layer are studied.

Stillman Visscher Jenks. Member of Co. A 339th infantry. (Polar Bear Expedition)

(Born in Kalamazoo on December 2, 1895. Died January 19, 1919 in Ust Padinga, Russia. Buried in White Chapel Cemetery, Troy, Michigan. Body brought back from Russia in 1929/30 (see Walter Dundon papers, Michael Macalla papers for more info)

The Pleistocene fauna of Hawver Cave /

Cover title.

A peculiar bear from Alaska,

Mode of access: Internet.

Request for assistance in preventing deaths and injuries from excavation cave-ins.

Mode of access: Internet.

Excavation and resource evaluation of sites 23PU2, 23PU255 and 23PU235 (Miller Cave complex), Fort Leonard Wood, Pulaski County, Missouri /

"For submission to U.S. Army Construction Engineering Research Laboratory, Champaign, Illinois."

Bear Valley radioactive mineral placers, Valley County, Idaho /

"October 1953."