This site pulls data from multiple different sources of data from the National Weather Service and the National Weather Service NOHRSC to create the easiest way to find the most accurate snowfall data in your area. This site attempts to correct that by combining and simplifying data from the National Weather Service and the NOAA. Weather websites are very good at reporting how much snow is forecast for the next day or week, but often make it difficult to see what the actual snowfall was at the end of the storm. In the 2020 census, the city's population density climbed to more than 48,300 inhabitants per square mile (18,600/km 2) of land, ranked fourth in the county behind Guttenberg, Union City and West New York. With more than 42,400 inhabitants per square mile (16,400/km 2) in data from the 2010 census, Hoboken was ranked as the third-most densely populated municipality in the United States among cities with a population above 50,000. The Census Bureau's Population Estimates Program calculated that the city's population was 57,703 in 2022, ranking the city as the 688th-most-populous in the country.
As of the 2020 United States census, the city's population was 60,419, an increase of 10,414 (+20.8%) from the 2010 census count of 50,005, which in turn reflected an increase of 11,428 (+29.6%) from the 38,577 counted in the 2000 census. Hoboken is part of the New York metropolitan area and is the site of Hoboken Terminal, a major transportation hub. Outcomes of such nonlinear interactions for future ecosystems will likely include changes in plant composition and productivity, dynamics of water balance, and availability of water resources.Hoboken is a city in Hudson County in the U.S. Unlike cold locations at high elevations or in the arctic, ecosystems at low elevations respond in a different and complex way to future conditions because of opposing effects of increasing water-limitation and a longer snow-free season. Our results suggest that big sagebrush and other similar semiarid ecosystems could decrease in viability or disappear in dry to medium areas and likely increase only in the snow-richest areas, i.e. Responses were sensitive to uncertainties in climatic prediction particularly, a shift of precipitation to the colder season could reduce impacts of a warmer and snow-poorer future, depending on the degree to which ecosystem phenology tracks precipitation changes. Beyond a threshold within this climatic gradient, predicted consequences for vegetation switched from no change to increasing transpiration. Our results suggest that effects on future ecosystem water balance will increase along a climatic gradient from dry, warm and snow-poor to wet, cold and snow-rich.
As a model system, we used simulation experiments to investigate big sagebrush ecosystems that dominate a large fraction of the semiarid western United States. Changes in water balance dynamics will be particularly pronounced at low elevations of mid-latitude dry regions because these areas will be the first to be affected by declining snow as a result of rising temperatures. A topic that has not been addressed with respect to declining snowpack is effects on ecosystem water balance. Widespread documentation of positive winter temperature anomalies, declining snowpack and earlier snow melt in the Northern Hemisphere have raised concerns about the consequences for regional water resources as well as wildfire.
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