Add to ORKGTemperature differences between Central Park and 20 stations in northern New Jersey for nights with strong radiational cooling during a lO-year period are evaluated. The effect of urbanization on temperature is strongest in the area adjacent to New York City, and diminishes with increasing distance from the metro-politan area. 1. INTRODUCT ION 2. PROCEDURE Urban areas tend to develop unique micro-climates different from more rural environ-ments. The concentration of people and industrial activity in urban areas increases temperature since greater local heat sources exist and nocturnal heat loss is often reduced. These temperatur
Long-term urban and rural climate data spanning January 1995 through October 2013 were analyzed to i...
We simulate the impact of impervious surface areas (ISA) on the U.S. local and regional climate. At ...
The urban heat island effect is a phenomenon observed worldwide, i.e. evening and nocturnal temperat...
Temperatllre differences between Central Park and 22 stations in northern New Jersey and sOlltheaste...
In this project, the urban heat island effect (UHI) was examined under current and projected climate...
Densely populated cities are experiencing Urban Heat Island (UHI) effects and localized hotspots. Ci...
This is a summary of a study that examined the urban heat island effect (UHI) of the greater Camden,...
The urban heat island (UHI) is a phenomenon that has been recognized since the turn of the 20th cent...
Temperatures in the cities are amplified through the urban heat island effect by an additional 2-4 ̊...
AbstractTemperatures in the cities are amplified through the urban heat island effect by an addition...
Along with urbanization, sealing of vegetated land and evaporation surfaces by impermeable materials...
Large cities account for a significant share of national population and wealth, and exert high press...
The term urban heat island (UHI) is used to describe the effect of urban temperatures rising several...
A previous study using temperature data to determine the magnitude of the New York City-Northern New...
Urban areas tend to have higher air temperatures than their surroundings as a result of man-made ait...
Long-term urban and rural climate data spanning January 1995 through October 2013 were analyzed to i...
We simulate the impact of impervious surface areas (ISA) on the U.S. local and regional climate. At ...
The urban heat island effect is a phenomenon observed worldwide, i.e. evening and nocturnal temperat...
Temperatllre differences between Central Park and 22 stations in northern New Jersey and sOlltheaste...
In this project, the urban heat island effect (UHI) was examined under current and projected climate...
Densely populated cities are experiencing Urban Heat Island (UHI) effects and localized hotspots. Ci...
This is a summary of a study that examined the urban heat island effect (UHI) of the greater Camden,...
The urban heat island (UHI) is a phenomenon that has been recognized since the turn of the 20th cent...
Temperatures in the cities are amplified through the urban heat island effect by an additional 2-4 ̊...
AbstractTemperatures in the cities are amplified through the urban heat island effect by an addition...
Along with urbanization, sealing of vegetated land and evaporation surfaces by impermeable materials...
Large cities account for a significant share of national population and wealth, and exert high press...
The term urban heat island (UHI) is used to describe the effect of urban temperatures rising several...
A previous study using temperature data to determine the magnitude of the New York City-Northern New...
Urban areas tend to have higher air temperatures than their surroundings as a result of man-made ait...
Long-term urban and rural climate data spanning January 1995 through October 2013 were analyzed to i...
We simulate the impact of impervious surface areas (ISA) on the U.S. local and regional climate. At ...
The urban heat island effect is a phenomenon observed worldwide, i.e. evening and nocturnal temperat...