scholarly journals Ecosystem services to enhance sustainable forest management in the US: moving from forest service national programmes to local projects in the Pacific Northwest

2017 ◽  
Vol 90 (5) ◽  
pp. 632-639 ◽  
Author(s):  
Robert L Deal ◽  
Nikola Smith ◽  
Joe Gates
Radiocarbon ◽  
2019 ◽  
Vol 61 (6) ◽  
pp. 1775-1784
Author(s):  
Helene Svarva ◽  
Pieter Grootes ◽  
Martin Seiler ◽  
Terje Thun ◽  
Einar Værnes ◽  
...  

ABSTRACTTo resolve an inconsistency around AD 1895 between radiocarbon (14C) measurements on oak from the British Isles and Douglas fir and Sitka spruce from the Pacific Northwest, USA, we measured the 14C content in single-year tree rings from a Scots pine tree (Pinus sylvestris L.), which grew in a remote location in Saltdal, northern Norway. The dataset covers the period AD 1864–1937 and its results are in agreement with measurements from the US Pacific coast around 1895. The most likely explanation for older ages in British oak in this period seems to be 14C depletion associated with the combustion of fossil fuels.


2016 ◽  
Vol 11 (1s) ◽  
pp. 1 ◽  
Author(s):  
Bruno De Cinti ◽  
Pierluigi Bombi ◽  
Fabrizio Ferretti ◽  
Paolo Cantiani ◽  
Umberto Di Salvatore ◽  
...  

This volume should be interpreted as a manual of best practices for sustainable forest management deriving from the experience of the project LIFE09ENV/IT/000078 ManFor C.BD coordinated by the National Research Council through the Institute of Agro-environmental and Forest Biology (CNR-IBAF). The other Project partners are: the Council for Agricultural Research and Economics (CREA), the University of Molise (UNIMOL), the Slovenian Forestry Institute (SFI) and the regions of Veneto and Molise. In addition, the National Centre for Forest Biodiversity of Verona and the Regional Office to biodiversity of Castel di Sangro of the Italian National Forest Service (CFS), as well as the Slovenian Forest Service (SFS) collaborated to the project. This manual consists of several individual articles dealing with specific issues related to the project. These articles are conceptually organized into five categories that from the description of the project and of its activities arrive at providing operative indications for forestry operators.


1986 ◽  
Vol 1 (2) ◽  
pp. 41-43
Author(s):  
Evelyn L. Bull ◽  
Jack Ward Thomas ◽  
Kirk Horn

Abstract A questionnaire was sent to each Ranger District in the Pacific North-west Region of the USDA Forest Service to get information on present snag-management programs. Ninety-five percent of the responding Ranger Districts left snags at levels that ranged from 0.15 snags/ha (0 06/ac) to 12-15 snags/ha (5-6/ac) on all forested lands. Live trees were intentionally left as future snags on 93% of the Ranger Districts. Live trees were killed to create snags on 41% of the Ranger Districts. Management recommendations are made as to the kind of snags to leave and methods of maintaining them. West. J. Appl. For. 1:41-43, April 1986


2018 ◽  
Vol 9 (2) ◽  
pp. 785-795 ◽  
Author(s):  
Vicente Pérez-Muñuzuri ◽  
Jorge Eiras-Barca ◽  
Daniel Garaboa-Paz

Abstract. Two Lagrangian tracer tools are evaluated for studies on atmospheric moisture sources and pathways. In these methods, a moisture volume is assigned to each particle, which is then advected by the wind flow. Usual Lagrangian methods consider this volume to remain constant and the particle to follow flow path lines exactly. In a different approach, the initial moisture volume can be considered to depend on time as it is advected by the flow due to thermodynamic processes. In this case, the tracer volume drag must be taken into account. Equations have been implemented and moisture convection was taken into account for both Lagrangian and inertial models. We apply these methods to evaluate the intense atmospheric rivers that devastated (i) the Pacific Northwest region of the US and (ii) the western Iberian Peninsula with flooding rains and intense winds in early November 2006 and 20 May 1994, respectively. We note that the usual Lagrangian method underestimates moisture availability in the continent, while active tracers achieve more realistic results.


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