Geology topics

George Robinson

Publications and source records attributed to George Robinson.

3 recordsLinked to original sources

USGS2024

New York State climate impacts assessment chapter 05: Ecosystems

The people of New York have long benefited from the state's diversity of ecosystems, which range from coastal shorelines and wetlands to extensive forests and mountaintop alpine habitat, and from lakes and rivers to greenspaces in heavily populated urban areas. These ecosystems provide key services such as food, water, forest products, flood prevention, carbon storage, climate moderation, recreational opportunities, and other cultural services. This chapter examines how changes in climatic conditions across the state are affecting different types of ecosystems and the services they provide, and considers likely future impacts of projected climate change. The chapter emphasizes how climate change is increasing the vulnerability of ecosystems to existing stressors, such as habitat fragmentation and invasive species, and highlights opportunities for New Yorkers to adapt and build resilience.

New York↗

USGS2022

Radial growth decline of white spruce (Picea glauca) during hot summers without drought: Preliminary results from a study site south of a boreal forest border

If the modern climate trend continues for an additional 20–40 years, forests along the southern border of Canadian taiga may shift into new ranges of annual temperature and precipitation that are similar to the modern climate of central New York State, United States. Here we investigate the possible future response of white spruce ( Picea glauca (Moench) Voss) to a warmer climate by studying trees planted 90 years ago near the southern limit of their climate tolerance in central New York, 300 km south of the boreal forest where this species is prevalent. We employed high-frequency recording dendrometers to determine radial growth phenology of six mature white spruce trees during 2013–2017. The results demonstrate significant reductions in the length of radial growth periods inversely proportional to the number of hot days with air temperature exceeding 30 °C. During years with very hot summers, the start of radial growth began about 3 days earlier than the 2013–2017 average. However, in those same years, the end of radial growth was also about 17 days earlier resulting in a shorter (70 days versus 100 days) radial growth season. Abundant (350–500 mm) summer precipitation, which resulted in soil moisture values of 20%–30%, allowed us to dismiss drought as a factor. Instead, a likely cause of reduced radial growth was mean temperature that exceeded optimal growth ranges, exacerbated by temperature extremes in ranges that lead to photoinhibition. The latter case was evident in the two warmest growing seasons (2013 and 2017), marked by extended periods of high daytime temperature (>30 °C) followed by early cessation of radial growth independent of seasonal precipitation.

New York↗

USGS2015

Effects of extreme floods on trout populations and fish communities in a Catskill Mountain river

Summary 1. Extreme hydrologic events are becoming more common with changing climate. Although the impacts of winter and spring ﬂoods on lotic ecosystems have been well studied, the effects of summer ﬂoods are less well known. 2. The Upper Esopus Creek Basin in the Catskill Mountains, NY, experienced severe ﬂooding from Tropical Storm Irene on 28 August 2011, and peak discharges exceeded the 0.01 annual exceedance probability (>100 year ﬂood) in some reaches. Three years of ﬁsh community data from pre-ﬂood surveys at nine sites were compared to data from 2 years of post-ﬂood surveys to evaluate changes in ﬁsh communities and populations of brown trout ( Salmo trutta ) and rainbow trout ( Oncorhynchus mykiss ). 3. Basinwide, ﬁsh assemblages were not strongly impacted and appeared highly resilient to the effects of the ﬂood. Total density and biomass of ﬁsh communities were greater at most sites 10-11 months after the ﬂood than 1 month prior to the ﬂood while richness and diversity were generally unchanged. Community composition did not differ signiﬁcantly between years or between the pre-and post-ﬂood periods. 4. Although the density of mature brown trout was low at most sites (mean density = 146 ﬁsh ha-1), young-of-the-year brown trout reached their highest density (mean = 2312 ﬁsh ha-1) during 2012. In contrast, rainbow trout densities declined substantially during the 5-year study and the 2012 year class was small (mean density = 222 ﬁsh ha-1). 5. Late summer ﬂoods may be less damaging to stream ﬁsh communities than winter or spring ﬂoods as spawning activity is negligible and early life stages of many species are generally larger and less susceptible to displacement and mortality. Additionally, post-ﬂood conditions may be advantageous for brown trout recruitment.

Freshwater Biology↗