scholarly journals Short Communication: A Comparative Analysis of Municipal Urban Tree Inventories of Selected Major Cities in North America and Europe

2012 ◽  
Vol 38 (1) ◽  
pp. 24-30
Author(s):  
Julie Kjeldsen-Kragh Keller ◽  
Cecil Konijnendijk

Effective management of the urban forest calls for municipalities to have a tree inventory of their urban resource. The approach to urban forestry is rather different in Europe and North America, both in terms of background and culture. This contribution discusses similarities and differences in tree inventory practices, based on a pilot study of three major cities in North America (Toronto, Ontario, Canada; and Boston, Massachusetts and New York City, New York, U.S.) and three major cities in Northern Europe (Oslo, Norway; and Aarhus and Copenhagen, Denmark). The pilot study consisted of semi-structured expert interviews in each city, and an analysis of their tree inventories in terms of their level of detail, how they were undertaken, and how they have been used. Each of the cities, with exception of Oslo, had inventoried all of their street trees. Volunteers were only used in Boston and New York City. None of the cities had developed a management plan based on their tree inventory. The inventory had only been completely incorporated into the work order system in New York City and Toronto. This explorative study shows that more research is needed to investigate what subsequently happens to tree inventories in municipalities after they have been performed. Moreover, more work is needed to identify whether inventories are being utilized to their full advantage in terms of producing management plans. Some key themes for further research are described. The set up of this pilot study could serve as a format for comprehensive research.

2011 ◽  
Vol 46 (2-3) ◽  
pp. 201-207 ◽  
Author(s):  
Holly Hagan ◽  
David C. Perlman ◽  
Don C. Des Jarlais

2006 ◽  
Vol 67 (03) ◽  
pp. 375-380 ◽  
Author(s):  
Enrique Baca-García ◽  
Maria A. Oquendo ◽  
Jeronimo Saiz-Ruiz ◽  
J. John Mann ◽  
Jose de Leon

2017 ◽  
Vol 1 (suppl_1) ◽  
pp. 46-46
Author(s):  
D. Russell ◽  
S.L. Szanton ◽  
J.L. Feinberg ◽  
K.H. Bowles

2013 ◽  
Vol 39 (3) ◽  
pp. 503-507 ◽  
Author(s):  
Corey H. Basch ◽  
Danna Ethan ◽  
Sonali Rajan ◽  
Sandra Samayoa-Kozlowsky ◽  
Charles E. Basch

2006 ◽  
Vol 31 (5) ◽  
pp. 907-912 ◽  
Author(s):  
Sandro Galea ◽  
Nancy Worthington ◽  
Tinka Markham Piper ◽  
Vijay V. Nandi ◽  
Matt Curtis ◽  
...  

2014 ◽  
Vol 11 (5) ◽  
pp. 5462-5486 ◽  
Author(s):  
Nadia Islam ◽  
Jennifer Zanowiak ◽  
Laura Wyatt ◽  
Rucha Kavathe ◽  
Hardayal Singh ◽  
...  

2018 ◽  
Vol 175 ◽  
pp. 184-194 ◽  
Author(s):  
Sara Perl Egendorf ◽  
Zhongqi Cheng ◽  
Maha Deeb ◽  
Victor Flores ◽  
Anna Paltseva ◽  
...  

2012 ◽  
Vol 25 (19) ◽  
pp. 6721-6742 ◽  
Author(s):  
Richard Seager ◽  
Neil Pederson ◽  
Yochanan Kushnir ◽  
Jennifer Nakamura ◽  
Stephanie Jurburg

Abstract The precipitation history over the last century in the Catskill Mountains region that supplies water to New York City is studied. A severe drought occurred in the early to mid-1960s followed by a wet period that continues. Interannual variability of precipitation in the region is related to patterns of atmospheric circulation variability in the midlatitude east Pacific–North America–west Atlantic sector with no link to the tropics. Associated SST variations in the Atlantic are consistent with being forced by the anomalous atmospheric flow rather than being causal. In winter and spring the 1960s drought was associated with a low pressure anomaly over the midlatitude North Atlantic Ocean and northerly subsiding flow over the greater Catskills region that would likely suppress precipitation. The cold SSTs offshore during the drought are consistent with atmospheric forcing of the ocean. The subsequent wet period was associated with high pressure anomalies over the Atlantic Ocean and ascending southerly flow over eastern North America favoring increased precipitation and a strengthening of the Northern Hemisphere storm track. Neither the drought nor the subsequent pluvial are simulated in sea surface temperature–forced atmosphere GCMs. The long-term wetting is also not simulated as a response to changes in radiative forcing by coupled models. It is concluded that past precipitation variability in the region, including the drought and pluvial, were most likely caused by internal atmospheric variability. Such events are unpredictable and a drought like the 1960s one could return while the long-term wetting trend need not continue—conclusions that have implications for management of New York City’s water resources.


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