Remote Sensing Analyzing Landscape Trends on Agriculture, Introduced Exotic Grasslands and Riparian Ecosystems in Arid Regions of Mexico

Riparian Zones are considered biodiversity and ecosystem services hotspots. In arid environments, these ecosystems represent key habitats, since water availability makes them unique in terms of fauna, flora and ecological processes. Simple yet powerful remote sensing techniques were used to assess how spatial and temporal land cover dynamics, and water depth reflect distribution of key land cover types in riparian areas. Our study area includes the San Miguel and Zanjon rivers in Northwest Mexico. We used a supervised classification and regression tree (CART) algorithm to produce thematic classifications (with accuracies higher than 78%) for 1993, 2002 and 2011 using Landsat TM scenes. Our results suggest a decline in agriculture (32.5% area decrease) and cultivated grasslands (21.1% area decrease) from 1993 to 2011 in the study area. We found constant fluctuation between adjacent land cover classes and riparian habitat. We also found that water depth restricts Riparian Vegetation distribution but not agricultural lands or induced grasslands. Using remote sensing combined with spatial analysis, we were able to reach a better understanding of how riparian habitats are being modified in arid environments and how they have changed through time.


Introduction
Riparian ecosystems (RE) are considered critical environments, due to the goods and services they provide, for established and developing human populations around the world [1,2].Described as transition zones between aquatic and terrestrial environments, with high fluxes of material, water and energy [3][4][5], RE are often considered biodiversity hotspots [6,7] as well as ecosystem services hotspots [3,[8][9][10][11][12].However, human activities such as livestock ranching, agricultural development and urbanization could result in the modification and degradation of these systems, diminishing their capacity to sustain their ecological function and thus provide services in the future.
Only 0.1% to 0.5% of the surface covered by arid environments in northwestern Mexico and the Southwestern US are RE [5,13,14].Despite this, RE represent key habitats in arid environments, since the availability of water makes them unique in terms of their fauna, flora and ecological processes [15].However, since economic and human activities are highly dependent on the availability and quality of water, the RE in arid environments are often subject to high rates of change and modification [15,16].
Due to the accessibility of freshwater, two of the most common activities associated with riparian systems in arid lands are agriculture (crop yielding) and livestock ranching [17,18].Since these activities typically modify the systems where they occur, it is critical to monitor how much of the riparian habitat is used by them, as well as analyze the effects that these activities are having on the health and presence of riparian zones.
The San Miguel and the Zanjon Rivers (SMR and ZR), two sub-watersheds in arid Northwestern Mexico, have experienced RE modification.Native riparian vegetation has been replaced by extensive cultivations of exotic grasslands for cattle foraging [19][20][21][22] in the watershed and the establishment of agricultural fields on the side of riverbeds [23].The alterations of these landscapes has been ongoing for over 300 years [24].However, starting in the 1950s, the introduction of exotic species for forage, a boom in agriculture (both in area used and intensity of usage) and a subsequent increase in water extraction (usually by wells), have altered the landscape with greater intensity [23,25,26].
In this study, we conducted a historical analysis on the transitions between vegetation types on two sub-watersheds in arid Northwestern Mexico.Using the approach proposed in this paper, historical as well as contemporary land cover distribution maps of riparian vegetation were generated.

Addressing Landscape Dynamics on Riparian Vegetation
Land cover changes of riparian systems in the Southwestern US and Northwestern Mexico have been occurring constantly over the last centuries [14,17,[27][28][29][30].However, the monitoring of land cover change over extensive areas was extremely challenging and resource consuming until technological capabilities provided by remote sensing approaches were developed [15,31].In this study, we use land cover classification algorithms [32,33], coupled with post-classification change detection techniques [34,35], to map the magnitude and location of land cover change over two sub-watersheds in arid Northwestern Mexico.We also used spatial analysis techniques to determine water depth under the riverbed [36] and the previously generated land cover thematic maps to account for the effect of water depth on riparian vegetation and other key land cover types.
Our focus in the present work was to assess the transitions within the riparian, agricultural and grassland cover classes in our study area between 1993 and 2011, as well as examine the relationship between these land cover types and water depth.Our objectives were: (1) to quantify land cover changes on riparian zones in arid environments; and (2) to observe if land cover distributions are related to water depth, which is often modified by ground water pumping for agricultural purposes.

Materials and Methods
We utilized Landsat Thematic Mapper (TM) image data to generate thematic classification maps (for 1993, 2002 and 2011), followed by an accuracy assessment for each of the products generated.After this, a land cover change assessment was performed, to assess the primary conversions that occurred for: (1) the entire river basin; and (2) the main riparian corridor.Emphasis was paid to changes due to agricultural activities or other environmental conditions (such as ground water).Finally, we generated continuous surfaces of water depth on the river in order to analyze how this variable relates to the dynamics of key land cover types on the area influenced by the river.

Study Area
The study area is composed of the SMR and the ZR, two sub-watersheds of the Sonora watershed in Northwestern Mexico.The riparian systems are located northeast of the city of Hermosillo, between the coordinates 28 • 53 N-30 • 46 N latitude and 110 • 21.5 W-111 • 21.5 W longitude (Figure 1).The approximate extent of the study area is 9437 km 2 (around 30% of the entire area of the Sonoran watershed), and elevation above sea level ranges from approximately 200 m to 2000 m (at Sierra Azul).In this region, potential annual evapotranspiration is 2400 mm, the mean annual temperature is 21 and the mean annual precipitation is about 421 mm, with 70% of it occurring during the summer (June-August) monsoon [37].The ZR is cataloged as an ephemeral river, while the SMR has both ephemeral (in most of its extension) and perennial flow segments between Cucurpe and Fabrica de los Angeles.It is in one of these perennial segments on the SMR, where the hydrometric station "El Cajon" has measured water flow since 1974 [38].The mean annual runoff measured in this hydrometric station is 32.33 mm 3 .Since 1996, a decrease in water flow has been observed and in 2012 the annual runoff was 8.174 mm 3 [39].Information regarding geological parameters on the watershed can be found elsewhere [40].
The study area is composed of the SMR and the ZR, two sub-watersheds of the Sonora watershed in Northwestern Mexico.The riparian systems are located northeast of the city of Hermosillo, between the coordinates 28°53′N-30°46′N latitude and 110°21.5′W-111°21.5′Wlongitude (Figure 1).The approximate extent of the study area is 9437 km 2 (around 30% of the entire area of the Sonoran watershed), and elevation above sea level ranges from approximately 200 m to 2000 m (at Sierra Azul).In this region, potential annual evapotranspiration is 2400 mm, the mean annual temperature is 21 °C and the mean annual precipitation is about 421 mm, with 70% of it occurring during the summer (June-August) monsoon [37].The ZR is cataloged as an ephemeral river, while the SMR has both ephemeral (in most of its extension) and perennial flow segments between Cucurpe and Fabrica de los Angeles.It is in one of these perennial segments on the SMR, where the hydrometric station "El Cajon" has measured water flow since 1974 [38].The mean annual runoff measured in this hydrometric station is 32.33 mm 3 .Since 1996, a decrease in water flow has been observed and in 2012 the annual runoff was 8.174 mm 3 [39].Information regarding geological parameters on the watershed can be found elsewhere [40].According to Shreve and Wiggins (1964) [41], the SMR falls within the Arizona Uplands and the ZR is part of the Sonoran Desert Plains.The National Forest Inventory (NFI) lists Subtropical Scrub, Forest and Mesquite as the most dominate vegetation cover types in the SMR.Grasslands and Desert Scrubs are the most prominent covers in the ZR sub-watershed [42].
During the last three centuries, the main economic activities in the SMR and ZR sub-watersheds have been agriculture and cattle ranching [37,43].Cattle ranching activities became more intensive in both sub-watersheds in the 1950s when buffelgrass (Cenchrus ciliaris) was introduced [22].The presence of buffelgrass pastures in both areas represents a significant pressure on the river system, since pastures have been established in areas adjacent to the riparian habitats.Buffelgrass has been According to Shreve and Wiggins (1964) [41], the SMR falls within the Arizona Uplands and the ZR is part of the Sonoran Desert Plains.The National Forest Inventory (NFI) lists Subtropical Scrub, Forest and Mesquite as the most dominate vegetation cover types in the SMR.Grasslands and Desert Scrubs are the most prominent covers in the ZR sub-watershed [42].
During the last three centuries, the main economic activities in the SMR and ZR sub-watersheds have been agriculture and cattle ranching [37,43].Cattle ranching activities became more intensive in both sub-watersheds in the 1950s when buffelgrass (Cenchrus ciliaris) was introduced [22].The presence of buffelgrass pastures in both areas represents a significant pressure on the river system, since pastures have been established in areas adjacent to the riparian habitats.Buffelgrass has been documented, in the Sonoran Desert, to outcompete and displace native flora by invading adjacent areas where it was not planted [20][21][22].
Another factor impacting the area is the water provisioned to the city of Hermosillo (more than 800,000 habitants), especially due to the construction of the Abelardo L. Rodriguez dam and the drilling of wells to extract water for urban and agricultural use [23].

Image Classification and Change Detection
We chose to use Landsat TM image data because: (1) they provide an extensive historical record for most places on Earth; and (2) the sensor's proven capabilities regarding its use in land cover detection and change studies in arid and semiarid riparian systems [15,31].For this study, we conducted our analysis at intervals of approximately ten years (1993, 2002 and 2011) to analyze changes in riparian vegetation and areas associated with either agriculture (croplands) or cattle ranching.To generate each classification two Landsat TM images were used per year, one prior to and one post monsoon (summer rain), to leverage the phenological characteristics of vegetation as a classification element [15,44].Our study area is covered by two Landsat TM Scenes (Path 35-Row 39 and Path 35-Row 40) with the collection dates varying from year to year (Table 1).The images were obtained from the Earth Explorer platform, managed by the United States Geological Survey [45].The Landsat TM Surface Reflectance images (CDR) acquired were orthorectified and processed through the Landsat Ecosystem Disturbance Adaptive Processing System (LEDAPS) to reduce atmospheric noise [45][46][47].A 30-m resolution Digital Elevation Model (DEM) was acquired from the National Elevation Dataset archives maintained by the US geological Survey [45].To improve the quality of the DEM, we resampled it to correct for sinks and tops [36].

Development of Water Depth Surfaces
Ground water depth data were acquired from the regional ground water office of the National Water Commission (CONAGUA).We obtained the location and water static levels, collected between 2005 and 2013, for 665 wells (212 in the SMR and 453 in the ZR).We obtained readings for static water level in each well with various frequencies (from once a year to once every three years).Since water levels were tested around the same time each year, we proceeded to average the readings in order to obtain a representation of water depth per well in the study area for the period between 2005 and 2013.

Classification Scheme
To develop our classification scheme (Table 2) featuring the classes of interest for our analysis, we utilized a combined methodology.First, we used a method proposed by Anderson et al. (1976) [48] where land cover classes were described generally (Level 1 classes, e.g., water, scrub, forest, etc.) according to the capabilities of Landsat TM like sensors.In order to achieve greater detail in our classification, we made further subdivisions of classes using a classification scheme proposed by the Mexican National Forest Commission (CONAFOR) where they describe plant communities according to their physiognomic, floristic and ecologic characteristics [42].The class denoted as "Urban Area" was inserted after the automated classification was performed using aerial photos and historical datasets as a reference.This was done due to misclassification and the "Urban Area" being rather small.

Classification Model
There are multiple classification techniques available to create maps regarding land cover for a set of properly pre-processed remotely sensed datasets [34,35,49,50].We used a Classification and Regression Tree (CART) model approach to generate the land cover maps for our study [51][52][53].CART models have been shown to be accurate when classifying landscape imagery [54,55] and better than other techniques when classifying arid environments [15,44].Using a CART model, we generated land cover maps for each year of the study using the variables derived from the two Landsat TM images collected and the DEM (Table 3).
The supervised classification approach requires that the user extract variables from layers of spatial information (scenes of Landsat TM) and auxiliary information (DEM) as a prerequisite for obtaining thematic maps of land use [15,32].The set of derived variables and the DEM were rescaled and re-projected in order to generate a satisfactory and consistent vertical integration [35].A layer stack was generated resulting in a single image per year (1993, 2002 and 2011) for each Landsat scene (Path 35-Row 39 and Path 35-Row 40) containing all the information generated for a total of 69 layers per year.Finally, the stacks were clipped to the area of interest.
Using the "clipped variable stack", we proceeded to collect training points for each of the classes listed in our class scheme (Table 2) to run the classification models.

Variable Reference No. of Layers Description
Normalized Difference Vegetation Index (NDVI) [56] 2 The reflectance properties of vegetation (in the red and near infrared) are used to derive a productivity proxy [33,56,57] Soil Adjusted Vegetation Index (SAVI) [58] 2 Minimizes the effect of soil reflectance on the quality of information generated by incorporating a correction factor in the denominator of the classical equation of NDVI [58].
Enhanced Vegetation Index [59,60] 2 Optimizes the vegetation signal increasing its sensitivity in regions of high biomass and reducing atmospheric interference.These characteristics are used to help reduce the possible saturation of data that can be present with the NDVI [60].

Reflectance Landsat TM 12
Represented as a percentage.Obtained by dividing the energy reflected by a material in a certain wavelength by the incident energy [32].

Tasseled Cap [61] 12
Displays data that defines vegetation cover.Provides information on greenness, wetness and brightness of each pixel in the image [32].
Multitemporal Kauth-Thomas (MKT) [62] 12 Provides vegetation dynamics between two images using their reflectance.The analysis requires a layer stack containing the bands of the two scenes acquired for the same year.

Principal Components [62] 12
A statistical technique applied to remotely sensed data used to find the causes of variability in an image and sort these causes in order of importance [32].
Texture [63] 12 In this case the texture refers to a description of the spatial variability of tones found within a scene [32].
Elevation, Aspect and Slope USGS (NED) 3 Represents the topographic conditions of the area which are derived from the Digital Elevation Model (DEM).

Supervised Classification and Accuracy Assessment
Training datasets for each of the land cover types were generated [32].To do this, we collected samples: (1) in the field for each land cover class in the study area (collected during a field season in the study area); (2) using historical aerial photography provided by web services; and (3) from the Landsat imagery (only when the land cover was obvious, as in the case of water bodies or agriculture parcels).We collected between 60 and 150 samples per class in order to train our classification model.
After the training points were fed in to the classification model and the thematic classification maps were created, we used a confusion matrix to assess the accuracy of each classification map produced [34,64,65].To create the confusion matrices, we applied a stratified random sampling of 30 points per class over each classified thematic map (with the exception of water and bare soil classes where we used 15 points per class) and assessed the accuracy of the classification by comparing the map to reality (assessed with field visits and high spatial resolution aerial imagery).Finally, we obtained statistical measurements from the confusion matrix such as: (1) producer's and user's accuracy; (2) overall accuracy; and (3) the Kappa statistic [65].

Change Detection in the Watershed and along the Rivers
After joining the two sections of the watershed (the north and the south portions) to create a single classification, for each of the years covered in this study, we proceeded to perform a change detection analysis [66].Specifically, we used the thematic classifications to generate a post-classification change detection analysis [15,44]  Through this analysis we address changes on a 5 km buffer from the two main water streams present in the watershed (the SMR and ZR).Our main interest was to address total change produced by human activities as a main driver for land cover change.

Water Depth
To generate continuous surfaces regarding ground water depth, we used the Inverse Distance Weighting (IDW) interpolation approach [36].This method measures the weighted average between known measurements between nearby points giving the greatest weight to the nearest point [36].We considered this method to be optimal for our study area since well density in the riparian areas is high and the distance between wells is small.The following function describes the IDW: where Z(x) is the unknown value to be interpolated in x; Z i is the known value; d i is the distance; and ω i is the pondered value (Inverse square of the distance).
We specified a 30-m spatial resolution for the output to allow direct comparison to the Landsat TM classification and change detection outcomes.The continuous water depth surface was measured in meters.Since we did not obtain reliable piezometric level measurements for the southernmost portion of the watershed our datasets only cover from a latitude of 29 • 12 00" to the north.

Relationships between Water Depth and Land Cover along the River
Using a 5 km buffer around the main water stream present in both sub-watersheds, we analyzed how water depth relates to land cover distribution and change in the riparian areas.As a sampling approach we selected 20 polygons (larger than 3 Ha to obtain at least 33 pixels in each area), distributed throughout the watershed, for areas where Riparian Vegetation, Agriculture and Grassland Cultivated/Induced did not change between 2002 and 2011.We extracted another 40 polygons where Riparian Vegetation was present in 2002 (20 with water depth lower than 10 m and 20 where water depth was greater than or equal to 10 m).Finally, we conducted an analysis on these polygons comparing the water depth: (1) with the land cover types (using a simple ANOVA); and (2) changes in Riparian Vegetation.

Classification Accuracy
The overall accuracies for our classifications were greater than 78% for the three maps generated (Table 4, Figure 2).User's accuracy values ranged from 60% to 100% and producer's accuracy values ranged from 52% to 100%.These results fall within the acceptable range for accuracy [67] and the errors present are likely due to the spectral similarities of certain classes.Bare Soil was often confused with the Mesquite Woodland and Grasslands classes due to very low vegetation density in the desert leading to almost nonexistent vegetation reflectance.In addition, the Grasslands class was often confused with classes like Desert Scrub and Mesquite Woodland since the class often contained elements of those two types of vegetation as part of its structure.Most of the land cover classes were correctly classified for our three maps (Figure 3) this is likely due to their: (1) Unique reflectance characteristics; (2) Particular phenological cycles; and (3) Presence in areas with distinctive topographical characteristics (slope, aspect or elevation).The two classes that obtained the highest accuracies were the Forest (Oak and Oak/Pine) and Water classes.This was expected since these two types of features have unique characteristics.

Trends and Changes in the Riparian Areas (1993-2011)
Using the classification outputs and the 5 km buffer around the SMR and ZR, we calculated two statistics: (1) Total change per class through time; and (2) The change among classes through time focusing on the Agriculture, Riparian Vegetation and Grasslands classes [15,44].

Land Cover Trends along the Rivers
We proceeded to analyze the trends for the 5 km buffer around the SMR and ZR using the classified land cover maps (Table 5).We observed a general decrease in the Agriculture and Grasslands classes and a significant increase in the extent of the Subtropical and Desert Scrub classes.We also observed very little change in the Riparian Vegetation areas (Table 5).Bare Soil was often confused with the Mesquite Woodland and Grasslands classes due to very low vegetation density in the desert leading to almost nonexistent vegetation reflectance.In addition, the Grasslands class was often confused with classes like Desert Scrub and Mesquite Woodland since the class often contained elements of those two types of vegetation as part of its structure.Most of the land cover classes were correctly classified for our three maps (Figure 3) this is likely due to their: (1) Unique reflectance characteristics; (2) Particular phenological cycles; and (3) Presence in areas with distinctive topographical characteristics (slope, aspect or elevation).The two classes that obtained the highest accuracies were the Forest (Oak and Oak/Pine) and Water classes.This was expected since these two types of features have unique characteristics.

Land Cover Trends along the Rivers
We proceeded to analyze the trends for the 5 km buffer around the SMR and ZR using the classified land cover maps (Table 5).We observed a general decrease in the Agriculture and Grasslands classes and a significant increase in the extent of the Subtropical and Desert Scrub classes.We also observed very little change in the Riparian Vegetation areas (Table 5).Human activities have caused a drastic change in land cover throughout the SMR and ZR sub-watersheds.Some of the most important changes are related to the establishment and abandonment of agricultural fields (vineyards, pecan orchards, pastures and others), the cultivation of buffelgrass pastures and extensive cattle ranching activities [20,68].It is important to mention that changes in the area might be related to other factors such as climatic trends, species competition and water redistribution [68,69].
The previous results suggest two important trends.First, the extent of area used as agricultural land near the river has been decreasing.This is consistent with data suggesting that water is now being used for urban use rather than for agricultural purposes [68].This has led to restrictions on water for agriculture and the abandonment of activities along both rivers.Second, the observed decrease in area indicates that induced grasslands used as pastures are not as resilient or pervasive as suggested previously [20][21][22].This was expected since the maintenance of the pastures is often intensive [37] and the governmental programs that introduced them are no longer providing the means to implement more grasslands or maintain the current pastures [70].

Riparian Vegetation
Our results show that Riparian Vegetation is more prone to change than Subtropical/Succulent Scrub, Mesquite Woodland or Agriculture even though these classes most often converted to Riparian Vegetation (Table 6).These results were mostly expected since agricultural fields are often established (or abandoned) near the riparian areas.Riparian Vegetation has been experiencing structural changes to its plant community composition due to the encroachment of mesquite woodlands along the rivers and conversion to Subtropical/Succulent Scrub vegetation [71].Cultivated/Induced Grasslands Cultivated/Induced Grasslands are present due to cattle ranching activities and the necessity of ranchers to improve pastoral activities [37,70].Our results show conversion from this class to: Desert Scrub, Mesquite Woodland, Agriculture or Riparian Vegetation (Table 7).On the other hand, the classes most often converted to Cultivated/Induced Grasslands are Mesquite Woodlands, Desert Scrub and Agriculture.Due to the biological characteristics of the grasslands introduced in our study area [21], the dynamic exchange between this and the other classes mentioned above is expected and actively promoted by economic activities [70].It seems that the conditions for grassland prairie growth in the study area are not adequate to replace Riparian Vegetation and change the systems state [72].
We found a decrease of nearly 30% of the Agricultural area from 1993 to 2011.Other authors found similar trends in the area [68].Changes were explained as a social response to the reallocation of water from agricultural to urban use, which was reflected in the abandonment of farmland by small producers in the suburbs of the peri-urban areas of Hermosillo.The abandonment of agricultural areas is common in arid environments due to decrease in water availability [44].Abandoned areas tend to experience re-establishment of riparian mesquite and desert scrub.The results show a significant difference between Riparian Vegetation, Induced Grasslands and Agriculture in regard to water depth (ANOVA p < 0.01).Specifically, we found that Riparian Vegetation distributes in a much shallower water depth (mean = 9.9 m, CI 95% = 0-10.9m) than grasslands (mean = 48.3m CI 95% = 38.3-58.3m) and Agriculture (mean = 37.1 m CI 95% = 26.9-47.4m) (Figure 4).
The previous was expected since Riparian Vegetation is not characterized by very deep root systems even when the vegetation structure has been modified and some phreatophytes like Prosopis species are present.Even though the literature suggests that Riparian Vegetation will only be present at depths no greater than 7 m [71], it seems like some of the species present in these particular systems can reach deeper water sources.This confirms that grasslands are dependent on rainfall and upper soil humidity to trigger and maintain biological cycles [73].Agriculture in this region is dependent on irrigation rather than ground water depth (or even rainfall) [23,25,26].
According to our results, we observed a greater depth of water on the ZR than the SMR.Our results suggest that deeper groundwater is related to agricultural development (Figure 5).We found that 70% of agricultural fields are associated with areas where groundwater depth is greater than 29 m.On the other hand, about 68% of the area covered by Riparian Vegetation in both sub-watersheds is associated with water depths of between 1 to 20 meters.Due to water extraction practices leading to the lowering of the ground water levels, agricultural areas that were previously RE have potentially crossed water depth thresholds necessary for the riparian vegetation to reestablish [71].
of water from agricultural to urban use, which was reflected in the abandonment of farmland by small producers in the suburbs of the peri-urban areas of Hermosillo.The abandonment of agricultural areas is common in arid environments due to decrease in water availability [44].Abandoned areas tend to experience re-establishment of riparian mesquite and desert scrub.The results show a significant difference between Riparian Vegetation, Induced Grasslands and Agriculture in regard to water depth (ANOVA p < 0.01).Specifically, we found that Riparian Vegetation distributes in a much shallower water depth (mean = 9.9 m, CI 95%= 0-10.9 m) than grasslands (mean = 48.3m CI 95% = 38.3-58.3m) and Agriculture (mean = 37.1 m CI 95% = 26.9-47.4m) (Figure 4).The previous was expected since Riparian Vegetation is not characterized by very deep root systems even when the vegetation structure has been modified and some phreatophytes like Prosopis species are present.Even though the literature suggests that Riparian Vegetation will only be present at depths no greater than 7 m [71], it seems like some of the species present in these particular systems can reach deeper water sources.This confirms that grasslands are dependent on rainfall and upper soil humidity to trigger and maintain biological cycles [73].Agriculture in this region is dependent on irrigation rather than ground water depth (or even rainfall) [23,25,26].
According to our results, we observed a greater depth of water on the ZR than the SMR.Our results suggest that deeper groundwater is related to agricultural development (Figure 5).We found that 70% of agricultural fields are associated with areas where groundwater depth is greater than 29 m.On the other hand, about 68% of the area covered by Riparian Vegetation in both sub-watersheds is associated with water depths of between 1 to 20 meters.Due to water extraction practices leading to the lowering of the ground water levels, agricultural areas that were previously RE have potentially crossed water depth thresholds necessary for the riparian vegetation to reestablish [71].Our results show that riparian cover converted mostly to Subtropical/Succulent Scrub in areas where the ground water levels were shallower than seven meters (Table 9).This was expected according to our ground water depth maps (Figure 4).The portions of the rivers that have the shallowest ground water occur mostly in the upper latitudes of the SMR where the adjacent vegetation is mostly Subtropical/Succulent Scrub.Our results show that riparian cover converted mostly to Subtropical/Succulent Scrub in areas where the ground water levels were shallower than seven meters (Table 9).This was expected according to our ground water depth maps (Figure 4).The portions of the rivers that have the shallowest ground water occur mostly in the upper latitudes of the SMR where the adjacent vegetation is mostly Subtropical/Succulent Scrub.The class that converted most to Riparian Vegetation, in areas where the ground water levels were deeper than seven meters, was Agriculture (Table 10).This can be explained by the fact that agricultural fields are highly managed systems, independent of ground water depth.The conversion of Riparian Vegetation to Mesquite Woodlands was apparent during field work and has been reported in the literature [17].The change from Riparian Vegetation to phreatophytes with long and deep root systems, like Prosopis spp., might be a consequence of an increase in the depth of ground water [17,74].
Mesquite Woodland and Agriculture are the classes that converted most to Riparian Vegetation, a trend that seems to be unrelated to ground water depth.However, it seems that Riparian Vegetation might be able to persist in environments with ground water depths greater than 7 m when modified by vegetation from adjacent land cover types.Our results show a constant exchange between Mesquite Woodland and Riparian Vegetation this was expected since our field observations and the literature [17,29,75,76] indicate that mesquite dominated vegetation tend to replace or modify the structure of ecosystems including riparian habitats.
The net change in Riparian Vegetation using the 7 m threshold shows that riparian areas have not undergone significant reduction or increase.However, we believe that the functionality of the environment has been heavily modified.Based on a literature review [17,71,74,77,78] and field observations of exchange between Riparian Vegetation and Mesquite Woodlands we can say that mesquites are becoming common vegetation present on the rivers of this region.

Conclusions
This study addresses techniques and methodologies to use remote sensing products and derive tools for real applications regarding the study of riparian land cover in arid environments.Moreover, it highlights the usefulness of a classification and land cover change detection approach to obtain timely information for decision making in developing countries.
Specifically, in this study, we found evidence suggesting that threats to riparian habitats in arid environments might come from multiple human factors due to economic activities developed in specific areas.We were able to observe fluctuation in the riparian land cover with the introduction and implementation of nonnative grasses.We observed interchange between Mesquite Woodland, Subtropical/Succulent Scrub and Riparian Vegetation.We believe that further details of these interchanges might be exposed through the study of the relationship of vegetation types to factors such as ground water depth and climatic adaptation.
We were able to capture differences in distribution and change of land cover classes in relation to water depth.Our results agree with the idea that Riparian Vegetation distributes mostly in areas of shallow water (water depth less than 10 m).However, we also found that Riparian Vegetation might thrive in areas with deeper water depth than previously reported.As expected, land cover distribution, as a function of water depth, was key for Riparian Vegetation, but not for other land cover classes analyzed (Grassland Cultivated/Induced and Agriculture).
The RE in arid environments can be considered extremely diverse in terms of the number of species, processes, functions and usage (by humans) when compared to adjacent vegetation or land cover types.It is important to study these environments in arid lands; even though the area occupied by them is small, their importance is enormous for the life in these zones.Through remote sensing and spatial analysis we have been able to further our understanding on how "arid wetlands" interact with the environment and how they change through time.

Figure 1 .
Figure 1.Location of the study area.The Río San Miguel-Río Zanjon region is located in the central part of the state of Sonora, Mexico.

Figure 1 .
Figure 1.Location of the study area.The Río San Miguel-Río Zanjon region is located in the central part of the state of Sonora, Mexico.

Figure 2 .
Figure 2. Thematic map (left) derived from the CART model using Landsat TM scene (right) subproducts and ancillary datasets.

Figure 2 .
Figure 2. Thematic map (left) derived from the CART model using Landsat TM scene (right) sub-products and ancillary datasets.

Figure 3 .
Figure 3. Results of land cover land use classifications for 1993, 2002 and 2011.A 5 km buffer was overlaid on the main rivers in the region.

3. 2 .
Trends and Changes in the Riparian Areas (1993-2011) Using the classification outputs and the 5 km buffer around the SMR and ZR, we calculated two statistics: (1) Total change per class through time; and (2) The change among classes through time focusing on the Agriculture, Riparian Vegetation and Grasslands classes [15,44].

Figure 4 .
Figure 4. Land cover relationship to average water depth in the ZR and SMR sub-watersheds.Figure 4. Land cover relationship to average water depth in the ZR and SMR sub-watersheds.

Figure 4 .
Figure 4. Land cover relationship to average water depth in the ZR and SMR sub-watersheds.Figure 4. Land cover relationship to average water depth in the ZR and SMR sub-watersheds.

Figure 5 .
Figure 5. Well distribution from where water depth readings were collected (a) and 5 km buffer extraction; (b) of water depth surface (generated after IDW interpolation) along rivers.3.3.2.Changes in Riparian Vegetation (between 2002 and 2011) Related to Water Depth

Figure 5 .
Figure 5. Well distribution from where water depth readings were collected (a) and 5 km buffer extraction; (b) of water depth surface (generated after IDW interpolation) along rivers.

Table 1 .
Dates of the Landsat TM Scenes selected by year.

Table 2 .
Description of the types of land use-land cover used for the classification scheme.Areas of small-leaved shrubs that grow on alluvial soils that may include groups of thorny species.Within this class can be found species belonging to the genera Cercidium (Parkinsonia), Olneya, Condalia, Lycium, Opuntia and Fouquieria, among others.vegetation located on the banks of the riverbed.They are characterized by the presence of species that require favorable moisture conditions such as Populus sp.This class may present individuals of the gennus Prosopis.
Areas of vegetation mainly formed by shrubs or low, thorny trees.They are described as an ecological transition between the class of forest and thorny scrub.The main genera that can be observed are Ipomoea, Bursera and Acacia, to name a few.In regions of hills and middle elevations, Cercidium microphyllum, Opuntia sp., Carnegia gigantea and Lophocereus schottii are the dominant species.9Forest(Oak and Oak/Pine) F Areas of woody vegetation found in temperate or cold climates with higher humidity.The canopy cover of this class is observed in more than 10% of the area with heights up to 15 m high.10 Natural/Native Grassland GN Areas dominated by native grasses.Located mainly in the areas of transition between Forest-Subtropical Shrub and forest-Desert Scrub.

Table 3 .
Variables used in the land cover classification derived from Landsat spectral reflectance data and a Digital Elevation Model (DEM).

Table 4 .
Summary of the User's, Producer's, Kappa and Overall accuracies for the CART (Classification and regression Tree) based vegetation classifications for 1993, 2002 and 2011.

Table 5 .
Land cover trends for the 5 km buffer in the ZR and SMR sub-watersheds.

Table 6 .
Land cover trends relative to the Riparian Vegetation class along the 5 km buffer in both sub-watersheds.

Table 9 .
Changes in riparian vegetation related to Water depth less than seven meters (changes from 2002 to 2011).

Table 10 .
Changes in Riparian Vegetation related to Water depth greater than seven meters (changes from 2002 to 2011).