Surface Soil Moisture Retrieval Using the L-Band Synthetic Aperture Radar Onboard the Soil Moisture Active-Passive Satellite and Evaluation at Core Validation Sites.

This paper evaluates the retrieval of soil moisture in the top 5-cm layer at 3-km spatial resolution using L-band dual-copolarized Soil Moisture Active-Passive (SMAP) synthetic aperture radar (SAR) data that mapped the globe every three days from mid-April to early July, 2015. Surface soil moisture retrievals using radar observations have been challenging in the past due to complicating factors of surface roughness and vegetation scattering. Here, physically based forward models of radar scattering for individual vegetation types are inverted using a time-series approach to retrieve soil moisture while correcting for the effects of static roughness and dynamic vegetation. Compared with the past studies in homogeneous field scales, this paper performs a stringent test with the satellite data in the presence of terrain slope, subpixel heterogeneity, and vegetation growth. The retrieval process also addresses any deficiencies in the forward model by removing any time-averaged bias between model and observations and by adjusting the strength of vegetation contributions. The retrievals are assessed at 14 core validation sites representing a wide range of global soil and vegetation conditions over grass, pasture, shrub, woody savanna, corn, wheat, and soybean fields. The predictions of the forward models used agree with SMAP measurements to within 0.5 dB unbiased-root-mean-square error (ubRMSE) and -0.05 dB (bias) for both copolarizations. Soil moisture retrievals have an accuracy of 0.052 m3/m3 ubRMSE, -0.015 m3/m3 bias, and a correlation of 0.50, compared to in situ measurements, thus meeting the accuracy target of 0.06 m3/m3 ubRMSE. The successful retrieval demonstrates the feasibility of a physically based time series retrieval with L-band SAR data for characterizing soil moisture over diverse conditions of soil moisture, surface roughness, and vegetation.

Microwave Radiometry at Frequencies From 500 to 1400 MHz: An Emerging Technology for Earth Observations.

Microwave radiometry has provided valuable spaceborne observations of Earth's geophysical properties for decades. The recent SMOS, Aquarius, and SMAP satellites have demonstrated the value of measurements at 1400 MHz for observing surface soil moisture, sea surface salinity, sea ice thickness, soil freeze/thaw state, and other geophysical variables. However, the information obtained is limited by penetration through the subsurface at 1400 MHz and by a reduced sensitivity to surface salinity in cold or wind-roughened waters. Recent airborne experiments have shown the potential of brightness temperature measurements from 500-1400 MHz to address these limitations by enabling sensing of soil moisture and sea ice thickness to greater depths, sensing of temperature deep within ice sheets, improved sensing of sea salinity in cold waters, and enhanced sensitivity to soil moisture under vegetation canopies. However, the absence of significant spectrum reserved for passive microwave measurements in the 500-1400 MHz band requires both an opportunistic sensing strategy and systems for reducing the impact of radio-frequency interference. Here, we summarize the potential advantages and applications of 500-1400 MHz microwave radiometry for Earth observation and review recent experiments and demonstrations of these concepts. We also describe the remaining questions and challenges to be addressed in advancing to future spaceborne operation of this technology along with recommendations for future research activities.

Vascular accumulation of a novel photosensitizer, MV6401, causes selective thrombosis in tumor vessels after photodynamic therapy.

The antivascular effects of photodynamic therapy (PDT) and their mechanisms are not clearly understood. Here, we examined the effects of PDT with a novel photosensitizer MV6401 on the microvasculature in a mammary tumor (MCaIV) grown in a murine dorsal skinfold chamber and in normal tissue controls. The mice were irradiated with light 15 min after i.v. administration of MV6401 when the drug was localized only in the vascular compartment, as shown by fluorescence microscopy and immunohistochemistry. PDT with MV6401 caused a dose-dependent biphasic blood flow stasis and vascular hyperpermeability, as determined by intravital microscopy. This biphasic response was classified into two components: (a) an acute response observed immediately after PDT; and (b) a long-term response observed at times greater than 3 h after PDT. The acute temporal vascular effects were characteristic of vasoconstriction but not of thrombus formation. However, the long-term vascular shutdown was mediated by thrombus formation, as evidenced by histological evaluation and inhibition with heparin. Minimal effects were observed in normal vessels after antivascular doses used against the tumor, but there was no long-term vascular damage. In concert with the stasis, a dose-dependent tumor growth delay was observed. This study provides mechanistic insights into antitumor vascular effects of PDT and suggests novel strategies for tumor treatment with PDT.

Targeting tumor vasculature and cancer cells in orthotopic breast tumor by fractionated photosensitizer dosing photodynamic therapy.

Photodynamic therapy (PDT) is a locally administered therapy currently being investigated in various clinical and preclinical settings. Tumor-host interaction is an important determinant of tumor biology and response to treatments. Here we report for the first time the effects of PDT on an orthotopic, murine mammary tumor model. PDT utilizes two individually nontoxic components: (a) the localization in the target site of a photosensitizing drug; and (b) the activation of the photosensitizer by light of an appropriate wavelength and energy. PDT after a single dose of the photosensitizer MV6401 induced drug dose-dependent, long-term blood flow shut down and tumor growth delay in the MCaIV tumor, grown in the mammary fat pad. The plasma half-life of MV6401 was approximately 20 min, and the drug was confined to the vascular compartment shortly after administration. However, it accumulated in the interstitial compartment at 2-6 h after the administration. Two equal MV6401 doses injected 4 h and 15 min before the light administration allowed the photosensitizer to localize in both vascular and tumor cell compartments. The fractionated drug dose PDT more effectively induced tumor growth delay than the same total dose given as a single dose either at 4 h or at 15 min before light administration. The long-term effect of the fractionated drug PDT on blood flow was also more extensive than single-dose PDT. Fractionated photosensitizer dosing PDT offers a new strategy to optimize PDT therapy.