Abstract

1992 to 2002 data from North American Regional Reanalysis (NARR) were used to investigate water budget on five land use areas: urban, forest, agriculture, lake, and wetland in the state of Florida, USA. The data were evaluated based on the anomalies of rainfall, evaporation, and soil moisture from the average condition. The anomalies were used to investigate the effect of extreme conditions on water budget parameters for various land uses in both northeast and south of Florida. The results showed that extreme events such as La Niña strongly affected the water budget on land-use areas in both regions as the negative monthly rainfall anomalies were observed during the 1999-2000 event, while EI Niño and thunderstorms in summer caused positive rainfall anomalies with more than 70% in all study areas. Higher rainfall led to higher soil moisture anomalies for the agriculture, forest, and wetland from 1992 to May 1998 in both study regions. However, soil moisture becomes primary source for evaporation in drier conditions, and differences in capacity of plants access water, often dictated by the rooting depth, can result in contrasting evaporative losses across vegetation types. Hence, the forest, which had the deeper roots, had lower soil moisture anomalies, but higher evaporation anomalies than agriculture area during the drought event.

Highlights

  • The catchment water cycle, assuming steady state, consists of precipitation (P), discharge (Q), and evapotranspiration (ET) [1]

  • Estimations of water cycle components include (1) atmosphere budget, which consists of sources and sinks as well as the transports between them, and (2) terrestrial water budget, which includes the soil moisture storage, surface/subsurface runoff, precipitation, and evapotranspiration [2]

  • Better understanding of the terrestrial water budget would improve our knowledge of the current climate, global hydrological cycle, and its dynamics and improve our skills in modeling, foresting, and analyzing the landatmosphere system

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Summary

Introduction

The catchment water cycle, assuming steady state, consists of precipitation (P), discharge (Q), and evapotranspiration (ET) [1]. Estimations of water cycle components include (1) atmosphere budget, which consists of sources (surface evaporation and evapotranspiration) and sinks (rainfall and cloud) as well as the transports between them, and (2) terrestrial water budget, which includes the soil moisture storage, surface/subsurface runoff, precipitation, and evapotranspiration [2]. Terrestrial and atmospheric water cycles are intrinsically coupled and linked through evapotranspiration and precipitation [3,4,5]. Humans are an active and increasingly significant component of the hydrologic cycle [7]. Better understanding of the terrestrial water budget would improve our knowledge of the current climate, global hydrological cycle, and its dynamics and improve our skills in modeling, foresting, and analyzing the landatmosphere system

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