CONTENT 2à(7)à2014

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GEOGRAPHY

Research Associate, Sergeev Institute of Environmental Geoscience RAS (IEG RAS); Ulansky pereulok 13, building 2, P.O.Box 145 101000, Moscow, Russia
Phone: +7-495-624-7257
E-mail: masha-a@yandex.ru
Corresponding author

Abstract:
We studied the change of forestland in the Central Russian Upland within the deciduous forest, forest-steppe, and steppe zones using old maps (XVIIIÖXXàcc.) and current satellite images. The forest distribution within the Central Russian Upland has been relatively stable during the last 220 years. On average, the decrease in the forested area was small. However, we identified significant changes in certain regions. In the southern part of CRU, the significant increase of the forested land is caused by the forest protection of abatis woodland and afforestation. During the last 100 years, reforestation took place mainly in the Oka basin due to both afforestation and natural reforestation. New forests appeared generally in ravines within all zones. The analysis of the abatis forests changes from the XVIII to XXàcc. allowed us to identify forested area within the Central Russian Upland prior to active development.
Key words: forestland, forest dynamic, Central Russian Upland, human impact

ENVIRONMENT

Hanna K.àLappalainen

Department of Physics, University of Helsinki, Helsinki, Finland
Finnish Meteorological Institute, Helsinki, Finland
E-mail: hanna.k.lappalainen@helsinki.fi
Corresponding author

Tuukka Petôjô

Department of Physics, University of Helsinki, Helsinki, Finland
E-mail: tuukka.petaja@helsinki.fi

Joni Kujansuu

Department of Physics, University of Helsinki, Helsinki, Finland
E-mail: joni.kujansuu@helsinki.fi

Veli-Matti Kerminen

Department of Physics, University of Helsinki, Helsinki, Finland
E-mail: veli-matti.kerminen@helsinki.fi

Anatoly Shvidenko

International Institute for Applied Systems Analysis (IIASA), Laxenburg, Austria
E-mail: shvidenk@iiasa.ac.at

Jaana Bôck

Dept of Forest Ecology University of Helsinki, Helsinki, Finland
E-mail: jaana.back@helsinki.fi

Timo Vesala

Department of Physics, University of Helsinki, Helsinki, Finland
E-mail: timo.vesala@helsinki.fi

Timo Vihma

Finnish Meteorological Institute, Helsinki, Finland
E-mail: Timo.Vihma@fmi.fi

Gerrit de Leeuw

Department of Physics, University of Helsinki, Helsinki, Finland
Finnish Meteorological Institute, Helsinki, Finland
E-mail: gerrit.leeuw@fmi.fi

Antti Lauri

Department of Physics, University of Helsinki, Helsinki, Finland
E-mail: antti.lauri@helsinki.fi

Taina Ruuskanen

Department of Physics, University of Helsinki, Helsinki, Finland
E-mail: taina.ruuskanen@helsinki.fi

Vladimir B.àLapshin

ROS HYDRO MET, Russia
E-mail: director@ipg.geospace.ru

Nina Zaitseva

Department of Earth Sciences, Russian Academy of Sciences, Russia
E-mail: ninaz40@rambler.ru

Olga Glezer

Institute of Geography RAS, Moscow, Russia

Mikhail Arshinov

Institute of Atmospheric Optics SB RAS, Tomsk, Russia
E-mail: michael@iao.ru
E-mail: mgg@iao.ru

Dominick V.àSpracklen

School of Earth and Environment, University of Leeds, Leeds, UK
E-mail: D.V.Spracklen@leeds.ac.uk

Steve R.àArnold

School of Earth and Environment, University of Leeds, Leeds, UK
E-mail: S.Arnold@leeds.ac.uk

Sirkku Juhola

Dept.of Environmental Sciences, University of Helsinki, Helsinki, Finland
E-mail: sirkku.juhola@helsinki.fi

Heikki Lihavainen

Finnish Meteorological Institute, Helsinki, Finland
E-mail: Heikki.Lihavainen@fmi.fi

Yrj? Viisanen

Finnish Meteorological Institute, Helsinki, Finland
E-mail: Yrjo.Viisanen@fmi.fi

Natalia Chubarova

Lomonosov Moscow State University, Moscow, Russia
E-mail: natalia.chubarova@gmail.com

Sergey Chalov

Lomonosov Moscow State University, Moscow, Russia

Nikolay Filatov

Northern Water Problems Institute, Karelian Research Center of RAS (NWPI)

Andrey Skorokhod

A.M.Obukhov Institute of Atmospheric Physics RAS, Moscow, Russia
E-mail: skorokhod@ifaran.ru

Nikolay Elansky

A.M.Obukhov Institute of Atmospheric Physics RAS, Moscow, Russia

Egor Dyukarev

Institute of Monitoring of Climatic and Ecological Systems SB RAS, Tomsk, Russia
E-mail: egor@imces.ru

Igor Esau

Nansen Environmental and Remote Sensing Centerà/ Bjerknes Centre for Climate Research, Bergen, Norway
E-mail: igor.ezau@nersc.no

Pertti Hari

Dept of Forest Ecology University of Helsinki, Helsinki, Finland
E-mail: pertti.hari@helsinki.fi

Vladimir Kotlyakov

Institute of Geography RAS, Moscow, Russia
E-mail: direct@igras.ru

Nikolay Kasimov

Lomonosov Moscow State University, Moscow, Russia
E-mail: secretary@geogr.msu.ru

Valery Bondur

AEROCOSMOS Research Institute for Aerospace Monitoring, Moscow, Russia
E-mail: vgbondur@aerocosmos.info

Gennady Matvienko

Institute of Geography RAS, Moscow, Russia

Alexander Baklanov

World Meteorological Organization,Genøve, Switzerland
Danish Meteorological Institute, Copenhagen, Denmark
E-mail: abaklanov@wmo.int
E-mail: alb@dmi.dk

Evgeny Mareev

Dept. of Radiophysics, Nizhny Novgorod State University, Nizhny Novgorod, Russia
E-mail: evgeny.mareev@gmail.com

Yuliya Troitskaya

Dept. of Radiophysics, Nizhny Novgorod State University, Nizhny Novgorod, Russia
E-mail: yalog@rambler.ru

Aijun Ding

Institute for Climate and Global Change Researchà& School of Atmospheric Sciences, University of Nanjing, China
E-mail: dingaj@nju.edu.cn

Huadong Guo

Institute of Remote Sensing and Digital Earth, Chinese Academy of Sciences, Beijing, China
E-mail: hdguo@ceode.ac.cn

Sergej Zilitinkevich

Department of Physics, University of Helsinki, Helsinki, Finland
Finnish Meteorological Institute, Helsinki, Finland
Dept. of Radiophysics, Nizhny Novgorod State University, Nizhny Novgorod, Russia
E-mail: sergej.zilitinkevich@fmi.fi
E-mail: sergej.zilitinkevich@fmi.fi

Markku Kulmala

Department of Physics, University of Helsinki, Helsinki, Finland
E-mail: markku.kulmala@helsinki.fi

Abstract:
The Pan-Eurasian Experiment (PEEX) is a new multidisciplinary, global change research initiative focusing on understanding biosphere-ocean-cryosphere-climate interactions and feedbacks in Arctic and boreal regions in the Northern Eurasian geographical domain. PEEX operates in an integrative way and it aims at solving the major scientific and society relevant questions in many scales using tools from natural and social sciences and economics. The research agenda identifies the most urgent large scale research questions and topics of the land-atmosphere-aquatic-anthropogenic systems and interactions and feedbacks between the systems for the next decades. Furthermore PEEX actively develops and designs a coordinated and coherent ground station network from Europe via Siberia to China and the coastal line of the Arctic Ocean together with a PEEX-modeling platform. PEEX launches a program for educating the next generation of multidisciplinary researcher and technical experts. This expedites the utilization of the new scientific knowledge for producing a more reliable climate change scenarios in regional and global scales, and enables mitigation and adaptation planning of the Northern societies. PEEX gathers together leading European, Russian and Chinese research groups. With a bottom-up approach, over 40 institutes and universities have contributed the PEEX Science Plan from 18 countries. In 2014 the PEEX community prepared Science Plan and initiated conceptual design of the PEEX land-atmosphere observation network and modeling platform. Here we present the PEEX approach as a whole with the specific attention to research agenda and preliminary design of the PEEX research infrastructure.
Key words: climate change, air quality, the Arctic, boreal forest, the Arctic Ocean, atmosphere-biosphere-cryosphere interactions, permafrost, greenhouse gases, anthropogenic influence, natural hazards, research infrastructures

Yurij K.àVasilÒchuk

Department of Landscape Geochemistry and Soil Geography, Lomonosov Moscow State University
E-mail: vasilch@geol.msu.ru
E-mail: vasilch_geo@mail.ru
Corresponding author

Alla C.àVasilÒchuk

Laboratory of Geoecology of the North, Lomonosov Moscow State University
E-mail: alla-vasilch@yandex.ru

Nadine A.àBudantseva

Department of Landscape Geochemistry and Soil Geography, Lomonosov Moscow State University
E-mail: nadin.budanceva@mail.ru

Julia N.àChizhova

Department of Landscape Geochemistry and Soil Geography, Lomonosov Moscow State University
E-mail: eacentr@yandex.ru

Wolfgang Papesch

ARC Seibersdorf research GmbH, Abt. Umweltforschung, Seibersdorf, Austria
E-mail: wolfgang.papesch@arcs.ac.at

Yevgenij Ye.àPodborny

Center for Hydro-Ecological Research, St. Petersburg
E-mail: podborniy@yandex.ru

Abstract:
The origin of the massive ice is important for understanding the Quaternary history of the Yamal region and to predict the occurrence of massive ice, which is important for gas exploration and the development of infrastructure. Massive ice bodies occur in the Bovanenkovo gas field area within sediments such as layers, laccoliths, rods and lenses. Maximal thickness of the tabular ice is 28.5àm; mean thickness is about 8àm. Deposits of the third terrace underlying and overlapping the tabular ice had been formed from 25àkaàBP to 20àkaàBP, according to ¹⁴C dates. Oxygen-isotope values (δ¹⁸O) of massive ices are ranged from 12.49àÉ up to -22.95àÉ. Deuterium (δD) values vary from -91.7àÉ up to -177.1àÉ. Deuterium excess (d_exc) changes from 3.4 to 10.6àÉ. Both homogenous and contrast distribution δ¹⁸O and (δD) vs. depths in massive ice bodies evidences the segregated and/or infiltrated-segregated manner of ice formation. Pollen, spores and algae spectra from ice are similar to pollen characteristics of modern lacustrine and coastal floodplain sediments in the area. The ingression of cold seawaters on a coastal flood plain caused freezing and ice segregation, with the formation of extensive ice layers under the large but shallow lakes. As a result, syngenetic and genetically heterogeneous ice, such as: segregated, infiltrated-segregated, lake bottom congelation ice etc. was formed.
Key words: massive ice, stable isotope composition, pollen, ¹⁴C age, Yamal Peninsula

Ekaterina Yu.àZhdanova

Faculty of Geography, Lomonosov Moscow State University, Moscow, Russia
Leninskie gory, 1, 1199911
Phone: +7-495-939-2337
E-mail: ekaterinazhdanova214@gmail.com
Corresponding author

Natalia Ye.àChubarova

Faculty of Geography, Lomonosov Moscow State University, Moscow, Russia
Leninskie gory, 1, 1199911
Phone: +7-495-939-2337
E-mail: chubarova@geogr.msu.ru

Mario Blumthaler

Division for Biomedical Physics of the Medical University of Innsbruck, Austria
E-mail: mario.blumthaler@i-med.ac.at

Abstract:
The paper contains the analysis of long-term measurements of erythemally weighted UV-radiation (Q_er) at the Meteorological Observatory of Moscow State University over the 1999Ö2013 period. Main features of seasonal variability of Q_er as well as the Q_er dependence on different geophysical parameters are studied. We showed that the average annual Q_er attenuation due to cloudiness, total ozone content, and aerosols, is about 29, 30%, and 7%, respectively. The maximal loss of Q_er due to cloudiness is observed in November (48%), while ozone-dependent attenuation is maximal in February-March (44%). We used the original technique to assess the UV-radiation impact on human health in Moscow. Specifically, we have identified the UV potential for the erythema formation and synthesis of vitamin D in humans with different skin types. The UV-deficiency conditions are observed for all considered skin types (1Ö4) during all days from November to February. The probability of the UV-optimum conditions for different skin types was assessed. It was shown, for example, that for skin type 2, the UV-optimum conditions are dominant from March to April and from September to October (maximum in September - 60%). We have also identified the periods with UV-excess conditions. For skin type 2, these conditions may exist from April to August.
Key words: UV-radiation, erythemal dose, skin type, vitamin D, UV-resources, Moscow

SUSTAINABILITY

Devon R.àDublin

Graduate School of Environmental Science, Hokkaido University, Kita 9 Nishi 8, Sapporo, 060-0809 Hokkaido, Japan
Phone: +818045080421
E-mail: devdub@ees.hokudai.ac.jp
Corresponding author

Noriyuki Tanaka

Center for Sustainability Science (CENSUS), Hokkaido University, Kita 9 Nishi 8, Sapporo, 060-0809 Hokkaido, Japan
Phone: +81117064532
E-mail: norit@census.hokudai.ac.jp

Abstract:
Satoyama is a Japanese term for landscapes that comprise a mosaic of different ecosystems which include forests, agricultural lands, grassland irrigation ponds and human settlements aimed at promoting viable human nature interaction. The Japanese government is seeking to revitalize it locally and promote it internationally, receiving accreditation as UNESCO Satoyama Initiatives. Here we explore the dynamics of this system and how it can be used as a model for any intended agricultural development in indigenous communities globally. In this paper we strongly address sustainable agriculture development which takes into consideration the local culture and traditions which exists.
Key words: satoyama, indigenous agriculture, sustainable development, landscape use, nature conservation

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